<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-32906434</id><updated>2011-10-04T13:46:05.244-04:00</updated><category term='Environmental News'/><category term='Geology Videos'/><title type='text'>GPC Geology Blog</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>98</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-32906434.post-5003586530781719187</id><published>2011-09-27T14:23:00.000-04:00</published><updated>2011-09-27T14:23:25.656-04:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Environmental News'/><title type='text'>All Owls are Equal, But Some are More Equal Than Others</title><content type='html'>This is a link to a post on&amp;nbsp;&lt;a href="http://geosciblog2.blogspot.com/"&gt;geosciblog - science&lt;/a&gt; on the issue of government vs. Barred Owls vs. Northern Spotted Owls.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5003586530781719187?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='related' href='http://geosciblog2.blogspot.com/2011/02/all-owls-are-equal-but-some-are-more.html' title='All Owls are Equal, But Some are More Equal Than Others'/><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5003586530781719187/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5003586530781719187' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5003586530781719187'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5003586530781719187'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2011/09/all-owls-are-equal-but-some-are-more.html' title='All Owls are Equal, But Some are More Equal Than Others'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2454686020167829160</id><published>2011-02-08T06:10:00.000-05:00</published><updated>2011-02-08T06:11:14.633-05:00</updated><title type='text'>A Minor Note Before Environmental Science Exam I</title><content type='html'>Remediate means to fix or clean up, as in an environmental problem.  Such as replanting a forest or cleaning up a pollution problem.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2454686020167829160?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2454686020167829160/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2454686020167829160' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2454686020167829160'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2454686020167829160'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2011/02/minor-note-before-environmental-science.html' title='A Minor Note Before Environmental Science Exam I'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5792831615825432126</id><published>2010-10-20T12:39:00.002-04:00</published><updated>2010-10-20T12:42:00.814-04:00</updated><title type='text'>Physical Geology Take Home Lab Assignment</title><content type='html'>You can click on the title or click &lt;a href="http://www.paccd.cc.ca.us/instadmn/physcidv/geol_dp/dndougla/SAND/SandExrc.htm"&gt;HERE&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;Answer then questions and turn these in next Wednesday (10/27).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5792831615825432126?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='related' href='http://www.paccd.cc.ca.us/instadmn/physcidv/geol_dp/dndougla/SAND/SandExrc.htm' title='Physical Geology Take Home Lab Assignment'/><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5792831615825432126/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5792831615825432126' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5792831615825432126'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5792831615825432126'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2010/10/physical-geology-take-home-lab.html' title='Physical Geology Take Home Lab Assignment'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5360549145809356933</id><published>2010-08-20T22:05:00.002-04:00</published><updated>2010-08-20T22:10:15.494-04:00</updated><title type='text'>Topo Map Videos</title><content type='html'>From user: ccohengses&lt;br /&gt;&lt;br /&gt;&lt;object width="480" height="385"&gt;&lt;param name="movie" value="http://www.youtube.com/v/SymUFSwEm3c?fs=1&amp;amp;hl=en_US"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/SymUFSwEm3c?fs=1&amp;amp;hl=en_US" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="480" height="385"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;From user: chenyugin&lt;br /&gt;&lt;br /&gt;&lt;object width="480" height="385"&gt;&lt;param name="movie" value="http://www.youtube.com/v/dZa2w2O1rhI?fs=1&amp;amp;hl=en_US"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/dZa2w2O1rhI?fs=1&amp;amp;hl=en_US" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="480" height="385"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;From user: lgibson100&lt;br /&gt;&lt;br /&gt;&lt;object width="480" height="385"&gt;&lt;param name="movie" value="http://www.youtube.com/v/SkaXsSYKmw8?fs=1&amp;amp;hl=en_US"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/SkaXsSYKmw8?fs=1&amp;amp;hl=en_US" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="480" height="385"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5360549145809356933?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5360549145809356933/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5360549145809356933' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5360549145809356933'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5360549145809356933'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2010/08/topo-map-videos.html' title='Topo Map Videos'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4638300716626516342</id><published>2010-05-09T21:39:00.005-04:00</published><updated>2010-05-10T05:56:51.981-04:00</updated><title type='text'>A Late Reminder for the Physical Geology Lecture Final</title><content type='html'>Sorry I didn't get to finish the new Power Point review, a few more things to review are:&lt;br /&gt;&lt;br /&gt;The &lt;a href="http://facstaff.gpc.edu/~jsummero/GaGeolNotes2009c.ppt"&gt;New Georgia Geology Notes&lt;/a&gt;. The main thing to remember are the 4 Provinces and the basic rock types in each one.&lt;br /&gt;&lt;br /&gt;Valley &amp;amp; Ridge - Paleozoic Sedimentary Rocks.&lt;br /&gt;Blue Ridge - Igneous and Metamorphic Rocks - highest topography in the state.&lt;br /&gt;Piedmont - Igneous and Metamorphic Rocks - has more igneous rocks, e.g., the large granite bodies and the diabase dikes, which are the youngest igneous rocks in Georgia.&lt;br /&gt;Coastal Plain - Late Mesozoic and Cenozoic Sediments&lt;br /&gt;&lt;br /&gt;The Valley &amp;amp; Ridge, Blue Ridge, and Piedmont Provinces are all considered part of the Appalachian Mountains.&lt;br /&gt;&lt;br /&gt;On the Mass Wasting Chapter - the cause is when Gravity overcomes Cohesion and Friction. Oversteepening of slopes is when natural support at the bottom of a slope is removed by erosion or excavation.&lt;br /&gt;&lt;br /&gt;On the Surface Water Chapter - remember the definition of gradient, cut-bank erosion occurs on the outside of a meander bend, point bar deposition occurs on the inside of the meander. Oxbow lakes are cut-off meanders.  Also remember Base Level - when it drops, down-cutting occurs; when it rises, deposition occurs.&lt;br /&gt;&lt;br /&gt;On the Ground Water Chapter - remember the definitions of aquifer, the basics of well construction (reasons for grout and surface pad).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4638300716626516342?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4638300716626516342/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4638300716626516342' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4638300716626516342'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4638300716626516342'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2010/05/late-reminder-for-physical-geology.html' title='A Late Reminder for the Physical Geology Lecture Final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2728505874477225036</id><published>2010-04-18T23:12:00.003-04:00</published><updated>2010-04-19T08:55:15.574-04:00</updated><title type='text'>Brief Exam III Review</title><content type='html'>Sorry for the delays.&lt;br /&gt;&lt;br /&gt;1.  Non-foliated - no preferred orientation of minerals.  Marble and quartzite.&lt;br /&gt;&lt;br /&gt;2.  Preferred alignment of prismatic crystals or flat, platy minerals.  Phyllite, Schist, Gneiss.&lt;br /&gt;&lt;br /&gt;3.  Slate - phyllite - Schist.&lt;br /&gt;&lt;br /&gt;4.  Water promotes the more active movement of ions, causing more substantial mineral changes.&lt;br /&gt;&lt;br /&gt;5.  Regional and Contact.&lt;br /&gt;&lt;br /&gt;6.  Vulcan Quarry in Norcross.&lt;br /&gt;&lt;br /&gt;7.  Ductile - takes place in deep settings at higher temperatures, where the rocks are flexible enough to fold and not break.&lt;br /&gt;     Brittle - takes place closer to surface, where rocks are colder and tend to fault, fracture, or joint.&lt;br /&gt;&lt;br /&gt;8.  Protolith - the original rock which is altered by metamorphism.  Shale - slate.  Limestone - marble.&lt;br /&gt;&lt;br /&gt;9.  Calcite and Wollastonite.&lt;br /&gt;&lt;br /&gt;10.  Blue Ridge and Piedmont.&lt;br /&gt;&lt;br /&gt;11.  Schist.&lt;br /&gt;&lt;br /&gt;12. Relative Age Dating - using different geological principles to identify a series of events.&lt;br /&gt;&lt;br /&gt;13. Absolute Age Dating - using radiometric decay of selected isotopes to estimate geologic age of particular igneous rocks.&lt;br /&gt;&lt;br /&gt;14. Original orientation of sedimentary rocks - horizontal, also known as Original Horizontality, identified by Nicolas Steno. He also identified Superposition and Lateral Continuity.&lt;br /&gt;&lt;br /&gt;15. Angular Unconformity - layers below tilted or folded, layers above - horizontal.&lt;br /&gt;Nonconformity - sedimentary layers over igneous or metamorphic rocks.&lt;br /&gt;Disconformity - parallel layers above and below erosion surface.&lt;br /&gt;&lt;br /&gt;16. You can see all three types from Hopi Point, on the South Rim of the Grand Canyon.&lt;br /&gt;&lt;br /&gt;17. On slide #3, there is a Nonconformity with the Tapeats Sandstone overlying the Brahma Schist, not a Disconformity.&lt;br /&gt;&lt;br /&gt;18. James Hutton was responsible for Inclusions and Cross-cutting relationships. A xenolith is an example of an inclusion in an igneous rock. A fault is a cross-cutting relationship.&lt;br /&gt;&lt;br /&gt;19. The Hermit Shale is present at both the Grand Canyon and at Sedona, AZ.&lt;br /&gt;&lt;br /&gt;20. The Organ Rock Shale and the Moenkopi Formation are present at both Monument Valley and Canyonlands National Park.&lt;br /&gt;&lt;br /&gt;21. An Index Fossil is a fossil that is geographically widespread, with a short existence in the fossil record. William Smith first recognized them.&lt;br /&gt;&lt;br /&gt;22. Half-life is the time needed for half of a radioactive element to break down to its stable daughter product.&lt;br /&gt;&lt;br /&gt;23. An isotope is a variety of an element with one or more extra neutrons.&lt;br /&gt;&lt;br /&gt;24. The Cambrian Period marked the first widespread appearance of hard-shelled organisms.&lt;br /&gt;The end of the Permian Period marked a widespread mass-extinction, with the loss of 90 - 95% of marine species.&lt;br /&gt;The end of the Cretaceous Period marked the widespread mass-extinction of the dinosaurs and ammonites.&lt;br /&gt;&lt;br /&gt;25. The late part of the Triassic Period, when modern corals and dinosaurs appeared in the fossil record, was approximately 210 million years ago.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2728505874477225036?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2728505874477225036/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2728505874477225036' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2728505874477225036'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2728505874477225036'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2010/04/brief-exam-iii-review.html' title='Brief Exam III Review'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4732655870654622379</id><published>2009-12-02T07:15:00.005-05:00</published><updated>2009-12-02T07:34:58.298-05:00</updated><title type='text'>A Few More Environmental Thoughts</title><content type='html'>A few thoughts from Michael Crichton about Environmentalism as a "religion" (in that it is based upon emotions).&lt;br /&gt;&lt;br /&gt;[&lt;strong&gt;Important Note: Just because you disagree with an Environmentalist, that doesn't mean that you are anti-Environment or that you want polluted air, water, or food.  Disagreement is not hate.]  &lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Listen carefully to Michael Crichton's words.&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;&lt;object width="425" height="344"&gt;&lt;param name="movie" value="http://www.youtube.com/v/Vv9OSxTy1aU&amp;amp;color1=0xb1b1b1&amp;amp;color2=0xcfcfcf&amp;amp;hl=en_US&amp;amp;feature=player_embedded&amp;amp;fs=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowScriptAccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/Vv9OSxTy1aU&amp;color1=0xb1b1b1&amp;color2=0xcfcfcf&amp;hl=en_US&amp;feature=player_embedded&amp;fs=1" type="application/x-shockwave-flash" allowfullscreen="true" allowscriptaccess="always" width="425" height="344"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;Consider this with George Carlin's somewhat more crude viewpoints.&lt;br /&gt;&lt;br /&gt;&lt;object width="425" height="344"&gt;&lt;param name="movie" value="http://www.youtube.com/v/qOOc5yiIWkg&amp;amp;color1=0xb1b1b1&amp;amp;color2=0xcfcfcf&amp;amp;hl=en_US&amp;amp;feature=player_embedded&amp;amp;fs=1"&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;param name="allowScriptAccess" value="always"&gt;&lt;embed src="http://www.youtube.com/v/qOOc5yiIWkg&amp;color1=0xb1b1b1&amp;color2=0xcfcfcf&amp;hl=en_US&amp;feature=player_embedded&amp;fs=1" type="application/x-shockwave-flash" allowfullscreen="true" allowscriptaccess="always" width="425" height="344"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;The way we deal with environmental issues and natural disasters is through Logic, Good Science, Freedom (which yields creativity and entrepreneurship), an Understanding of Historical Perspective,...i.e., Sober, adult reactions, not "the sky is falling" hysteria.&lt;strong&gt;&lt;/strong&gt;&lt;strong&gt;&lt;/strong&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4732655870654622379?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4732655870654622379/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4732655870654622379' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4732655870654622379'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4732655870654622379'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/12/few-more-environmental-thoughts.html' title='A Few More Environmental Thoughts'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5059696294487192338</id><published>2009-11-28T16:58:00.006-05:00</published><updated>2009-11-28T17:04:51.339-05:00</updated><title type='text'>Suggestions for Physical Geology Lab Final</title><content type='html'>Be familiar with:&lt;br /&gt;&lt;br /&gt;Cleavage - which minerals have it, which don't.&lt;br /&gt;&lt;br /&gt;Igneous textures&lt;br /&gt;&lt;br /&gt;Metamorphic textures&lt;br /&gt;&lt;br /&gt;Sedimentary textures&lt;br /&gt;&lt;br /&gt;Law of "v"s regarding topo maps.&lt;br /&gt;&lt;br /&gt;More too come...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5059696294487192338?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5059696294487192338/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5059696294487192338' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5059696294487192338'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5059696294487192338'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/11/suggestions-for-physical-geology-lab.html' title='Suggestions for Physical Geology Lab Final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4074032696240974772</id><published>2009-11-15T20:35:00.002-05:00</published><updated>2009-11-15T20:46:42.034-05:00</updated><title type='text'>A few notes for Exam III, Environmental Science</title><content type='html'>Sorry for the delay, I was in Austin, TX for job training Wed. PM - Sat. AM..&lt;br /&gt;&lt;br /&gt;Important concepts to remember - Orographic Effect and Rain Shadow Effect.&lt;br /&gt;&lt;br /&gt;Plate Tectonics - Rift (Divergent) Zones, Subduction (Convergent) Zones, Transform Fault Zones, Isostacy, Difference between Continental crust and Oceanic crust.&lt;br /&gt;&lt;br /&gt;In Subduction zones, the melting of oceanic sediments, along with oceanic crust, provides some of the quartz that makes Andesitic volcanoes explosive.&lt;br /&gt;&lt;br /&gt;Basalts are erupted where the crust is thin or where there is a hot spot.&lt;br /&gt;&lt;br /&gt;Mount St. Helens is an example of a composite or stratovolcano.&lt;br /&gt;&lt;br /&gt;When shales and limestones are dark colored, that is a sign of them being organic-rich.&lt;br /&gt;&lt;br /&gt;Moisture and temperature are the most important factors in how rapidly soil forms from weathered rocks.  Warm and moist are the most favorable conditions.&lt;br /&gt;&lt;br /&gt;More may be added later...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4074032696240974772?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4074032696240974772/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4074032696240974772' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4074032696240974772'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4074032696240974772'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/11/few-notes-for-exam-iii-environmental.html' title='A few notes for Exam III, Environmental Science'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4740849960616784215</id><published>2009-10-03T10:08:00.002-04:00</published><updated>2009-10-03T10:11:11.186-04:00</updated><title type='text'>The Real Threats to Coral Atolls</title><content type='html'>Blaming human-caused global warming for damage to coral reefs is an exercise in laziness.  Here is an in-depth article about real threats to coral reefs, which when left alone, have survived past episodes of warming and cooling, of sea level rise and fall.&lt;br /&gt;&lt;br /&gt;[Click on the title for more info.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4740849960616784215?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='related' href='http://jennifermarohasy.com/blog/2009/09/the-real-threats-to-coral-atolls/#more-6457' title='The Real Threats to Coral Atolls'/><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4740849960616784215/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4740849960616784215' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4740849960616784215'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4740849960616784215'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/10/real-threats-to-coral-atolls.html' title='The Real Threats to Coral Atolls'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2964982162560978649</id><published>2009-10-01T07:46:00.002-04:00</published><updated>2009-10-01T07:52:45.593-04:00</updated><title type='text'>To the Physical Geology Lab Class...</title><content type='html'>Here are some needed links for your take-home exam.&lt;br /&gt;&lt;br /&gt;My home page: &lt;a href="http://facstaff.gpc.edu/~jsummero/"&gt;http://facstaff.gpc.edu/~jsummero/&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Temporary Assignment Page: &lt;a href="http://facstaff.gpc.edu/~jsummero/TempAssignmentPage.html"&gt;http://facstaff.gpc.edu/~jsummero/TempAssignmentPage.html&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Questions: &lt;a href="http://facstaff.gpc.edu/~jsummero/PhysicalGeologyLabMidterm09.doc"&gt;http://facstaff.gpc.edu/~jsummero/PhysicalGeologyLabMidterm09.doc&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;My Physical Geology webpage, scroll down for Power Point notes related to Minerals, Igneous Rocks, and Sedimentary Rocks: &lt;a href="http://facstaff.gpc.edu/~jsummero/PhysicalGeology2009.htm"&gt;http://facstaff.gpc.edu/~jsummero/PhysicalGeology2009.htm&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Sorry for missing class, by the time we were finished with my son's doctor visit, for the Type A flu, and then going to three drug stores to find the right medicine, it was too late to make it to class.&lt;br /&gt;&lt;br /&gt;This needs to be done by Lab time on Monday.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2964982162560978649?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2964982162560978649/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2964982162560978649' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2964982162560978649'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2964982162560978649'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/10/to-physical-geology-lab-class.html' title='To the Physical Geology Lab Class...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3464078205873891329</id><published>2009-09-18T16:26:00.003-04:00</published><updated>2009-09-18T16:27:41.467-04:00</updated><title type='text'>To the Environmental Science Class</title><content type='html'>Today I attempted to update the website from the Alpharetta campus, but as they didn't have the Microsoft FrontPage program, I was unable to do so.  Maybe I will try again tomorrow (Saturday), so perhaps check again tomorrow afternoon.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3464078205873891329?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3464078205873891329/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3464078205873891329' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3464078205873891329'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3464078205873891329'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/09/to-environmental-science-class.html' title='To the Environmental Science Class'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6295294751312008000</id><published>2009-09-11T16:26:00.001-04:00</published><updated>2009-09-11T16:28:01.169-04:00</updated><title type='text'>Website Updates</title><content type='html'>Sorry I didn't get the website updated, didn't get a chance to get to the Covington (or another of the GPC campuses).  Will try to get there early on Monday to update Chapter 3 and 4.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6295294751312008000?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6295294751312008000/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6295294751312008000' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6295294751312008000'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6295294751312008000'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/09/website-updates.html' title='Website Updates'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4645723795874661250</id><published>2009-09-08T05:58:00.003-04:00</published><updated>2009-09-08T06:02:53.133-04:00</updated><title type='text'>A Few Thoughts on the California Wildfires</title><content type='html'>&lt;a href="http://www.wnd.com/index.php?fa=PAGE.view&amp;amp;pageId=109050"&gt;Columnist Barbara Simpson &lt;/a&gt;has some thoughts about why the fires in California are so severe.  &lt;br /&gt;&lt;br /&gt;It is because of past tinkering with nature (as George Carlin suggested).  Some areas had not had a fire in 40 years, thus there was an overabundance of dead timber, dead and living undergrowth and once the fire got started (in this case by arson), there is little stopping it.&lt;br /&gt;&lt;br /&gt;[Disclaimer: World Net Daily is a bit "over-the-top" on some issues, so if you venture away from this column, you are on your own.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4645723795874661250?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4645723795874661250/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4645723795874661250' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4645723795874661250'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4645723795874661250'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/09/few-thoughts-on-california-wildfires.html' title='A Few Thoughts on the California Wildfires'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1925561390714654860</id><published>2009-08-19T11:46:00.003-04:00</published><updated>2009-08-19T11:48:32.073-04:00</updated><title type='text'>George Carlin on Global Warming</title><content type='html'>Language warning, George Carlin (and Penn &amp; Teller) recognize absurdity when they see it.  I don't agree with everything they ridicule, but once in a while, they "get it right".  So, be forewarned that there is "colorful" language in this video:&lt;br /&gt;&lt;br /&gt;&lt;object width="425" height="344"&gt;&lt;param name="movie" value="http://www.youtube.com/v/qOOc5yiIWkg&amp;hl=en&amp;fs=1&amp;"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/qOOc5yiIWkg&amp;hl=en&amp;fs=1&amp;" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="425" height="344"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;Again, this is being presented as a learning tool, without endorsement to all of the verbiage within.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1925561390714654860?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1925561390714654860/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1925561390714654860' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1925561390714654860'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1925561390714654860'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/08/george-carlin-on-global-warming.html' title='George Carlin on Global Warming'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5006164266060662650</id><published>2009-08-17T12:47:00.003-04:00</published><updated>2009-08-17T12:47:53.030-04:00</updated><title type='text'>Environmental Science Class</title><content type='html'>My intro/Rant, Chapter 1 Power Point and part of Chapter 2 Power Point are here:&lt;br /&gt;&lt;br /&gt;&lt;a href="http://facstaff.gpc.edu/~jsummero/EnvSciIndex2009.htm"&gt;http://facstaff.gpc.edu/~jsummero/EnvSciIndex2009.htm&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Will update more...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5006164266060662650?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5006164266060662650/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5006164266060662650' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5006164266060662650'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5006164266060662650'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/08/environmental-science-class.html' title='Environmental Science Class'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3958725749725805424</id><published>2009-07-28T07:56:00.003-04:00</published><updated>2009-07-28T09:12:53.541-04:00</updated><title type='text'>While the modem is working...</title><content type='html'>A few more suggestions.&lt;br /&gt;&lt;br /&gt;Remember what a &lt;strong&gt;gaining stream&lt;/strong&gt; is versus a &lt;strong&gt;losing stream&lt;/strong&gt;.&lt;br /&gt;&lt;br /&gt;For surface and ground water issues - remember what &lt;strong&gt;Capacity&lt;/strong&gt; vs. &lt;strong&gt;Competency&lt;/strong&gt; is about, what a &lt;strong&gt;Recharge Zone&lt;/strong&gt; is and what a &lt;strong&gt;Drainage Basin&lt;/strong&gt; (or Watershed) is.&lt;br /&gt;&lt;br /&gt;Other stuff - &lt;strong&gt;Disconformity&lt;/strong&gt; - horizontal layers, separated by an erosion surface - Redwall Limestone over Muav Limestone in Grand Canyon. &lt;strong&gt;Nonconformity&lt;/strong&gt; - sedimentary rocks over igneous/metamorphics - Chattahoochee gravels over saprolite or Tapeats Sandstone over metamorphics in Grand Canyon. &lt;strong&gt;Angular Unconformity&lt;/strong&gt; - Cambrian Tonto Group over tilted Grand Canyon Supergroup.&lt;br /&gt;&lt;br /&gt;Youngest igneous rocks in Ga. are the diabase dikes on the Piedmont.&lt;br /&gt;&lt;br /&gt;Soils to remember - Pedalfers - this area; Laterites - tropical rain forests; Pedocals - El Paso area.&lt;br /&gt;&lt;br /&gt;Remember shield volcanoes - usually hot spots or rift zones.  Composite volcanoes - usually inland from subduction zones.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3958725749725805424?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3958725749725805424/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3958725749725805424' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3958725749725805424'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3958725749725805424'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/07/while-modem-is-working.html' title='While the modem is working...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7660215702223490024</id><published>2009-07-27T15:58:00.002-04:00</published><updated>2009-07-27T16:05:19.583-04:00</updated><title type='text'>More study suggestions for the final</title><content type='html'>Most of the metamorphic rocks on the Ga. Piedmont and Blue Ridge were &lt;strong&gt;regionally metamorphosed&lt;/strong&gt;, the only places to see contact metamorphism is close to the large granites and the diabase dikes.&lt;br /&gt;&lt;br /&gt;Remember the difference between &lt;strong&gt;foliated &lt;/strong&gt;and &lt;strong&gt;non-foliated metamorphic rocks&lt;/strong&gt; and remember examples of each.&lt;br /&gt;&lt;br /&gt;The agents of metamorphism are &lt;strong&gt;heat, pressure, and fluids (pressurized water).&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Igneous and metamorphic activity &lt;/strong&gt;are &lt;strong&gt;Internal Processes (happening below the Earth's surface), &lt;/strong&gt;while &lt;strong&gt;Weathering, Erosion, and Deposition&lt;/strong&gt; are &lt;strong&gt;External Processes (happening at the Earth's surface).&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;The grain sizes of clastic sedimentary rocks are related to &lt;strong&gt;Water Energy Conditions.  &lt;/strong&gt;The amount of sorting is related to water energy and length of transport.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7660215702223490024?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7660215702223490024/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7660215702223490024' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7660215702223490024'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7660215702223490024'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/07/more-study-suggestions-for-final.html' title='More study suggestions for the final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5850997941402785632</id><published>2009-07-27T09:09:00.003-04:00</published><updated>2009-07-27T09:12:00.036-04:00</updated><title type='text'>Some study suggestions will follow</title><content type='html'>I have been having trouble with my home DSL modem.  Will add some more suggestions for later.&lt;br /&gt;&lt;br /&gt;For now -&lt;br /&gt;&lt;br /&gt;Remember the four Ga. Geologic Provinces and characteristics, such as -&lt;br /&gt;&lt;br /&gt;Igneous &amp; Metamorphic - Blue Ridge and Piedmont&lt;br /&gt;Sedimentary - Valley &amp; Ridge and Coastal Plain&lt;br /&gt;&lt;br /&gt;Valley &amp; Ridge, Blue Ridge, and Piedmont are considered part of the Appalachians.&lt;br /&gt;&lt;br /&gt;Remember examples of Valley &amp; Ridge fossils vs. Coastal Plain fossils.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5850997941402785632?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5850997941402785632/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5850997941402785632' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5850997941402785632'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5850997941402785632'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/07/some-study-suggestions-will-follow.html' title='Some study suggestions will follow'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1696394252319860317</id><published>2009-07-23T14:30:00.002-04:00</published><updated>2009-07-23T14:34:55.112-04:00</updated><title type='text'>Exam IV</title><content type='html'>Here is the link to the page where the Exam can be downloaded.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://facstaff.gpc.edu/~jsummero/Take%20Home%20Exams.html"&gt;http://facstaff.gpc.edu/~jsummero/Take%20Home%20Exams.html&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1696394252319860317?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1696394252319860317/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1696394252319860317' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1696394252319860317'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1696394252319860317'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/07/exam-iv.html' title='Exam IV'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7666465569747465183</id><published>2009-07-22T23:16:00.002-04:00</published><updated>2009-07-22T23:21:52.524-04:00</updated><title type='text'>Links for Take Home Exam</title><content type='html'>&lt;a href="http://facstaff.gpc.edu/~pgore/geology/geo101/masswasting.html"&gt;Mass Wasting&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;a href="http://facstaff.gpc.edu/~pgore/geology/geo101/grndh2o.htm"&gt;Groundwater&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;a href="http://facstaff.gpc.edu/~pgore/geology/geo101/hydro2.htm"&gt;Surface Waters, Erosion, related subjects&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;a href="http://facstaff.gpc.edu/~pgore/geology/geo101/coastal.htm"&gt;Shoreline Processes&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;These should help with the questions.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7666465569747465183?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7666465569747465183/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7666465569747465183' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7666465569747465183'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7666465569747465183'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/07/links-for-take-home-exam.html' title='Links for Take Home Exam'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-8774798330932052894</id><published>2009-07-15T06:35:00.004-04:00</published><updated>2009-07-22T23:16:52.629-04:00</updated><title type='text'>A Few Review Suggestions for Exam III</title><content type='html'>Remember the 4 Ga. Provinces and their major characteristics, i.e.:&lt;br /&gt;&lt;ul&gt;&lt;li&gt;&lt;div align="justify"&gt;in which provinces do you find igneous &amp;amp; metamorphic rocks, &lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;div align="justify"&gt;in which provinces do you find fossils (and which types are highlighted),&lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;div align="justify"&gt;where are the granites and the diabase dikes,&lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;div align="justify"&gt;age ranges for the provinces&lt;/div&gt;&lt;/li&gt;&lt;/ul&gt;(Remember to work on your note sheets)&lt;br /&gt;&lt;br /&gt;Other stuff...&lt;br /&gt;&lt;br /&gt;What protolith/parent rock means regarding metamorphics.&lt;br /&gt;How snowball garnets form (regarding shearing).&lt;br /&gt;Angular unconformities/Disconformities/Nonconformities and example of Ang. Unconf. - in Grand Canyon - Tonto Group over Grand Canyon Supergroup and example of Nonconf. of river gravels over saprolite.&lt;br /&gt;Examples of foliated metamorphics - slate, phyllite, schist, gneiss.&lt;br /&gt;&lt;br /&gt;More will be added later.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-8774798330932052894?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/8774798330932052894/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=8774798330932052894' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8774798330932052894'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8774798330932052894'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/07/few-review-suggestions-for-exxam-iii.html' title='A Few Review Suggestions for Exam III'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4517982373568201095</id><published>2009-06-16T09:06:00.002-04:00</published><updated>2009-06-16T09:09:46.202-04:00</updated><title type='text'>Current Events</title><content type='html'>Even though this is not directly related to Physical Geology, as Geology is the study of the Earth (in a broad sense), &lt;a href="http://www.telegraph.co.uk/comment/columnists/christopherbooker/5525933/Crops-under-stress-as-temperatures-fall.html"&gt;this article&lt;/a&gt; on Global Cooling (which has been predicted for years by Russian solar scientists), should be of interest.&lt;br /&gt;&lt;br /&gt;FYI, here is &lt;a href="http://www.john-daly.com/history.htm"&gt;a link&lt;/a&gt; that describes the political origins of the Global Warming Hysteria (as it relates to carbon dioxide).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4517982373568201095?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4517982373568201095/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4517982373568201095' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4517982373568201095'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4517982373568201095'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/06/current-events.html' title='Current Events'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3476154518961093160</id><published>2009-05-10T23:06:00.003-04:00</published><updated>2009-05-10T23:16:14.290-04:00</updated><title type='text'>A Few More Notes...on Earthquakes and stuff</title><content type='html'>Though we didn't get to cover things related to earthquakes, if any questions come up on the first part of the test, a quick reminder...&lt;br /&gt;&lt;br /&gt;There are three types of earthquake seismic waves that reach the seismograph.  The P-waves (Primary Waves) are the fastest and reach the seismograph first.&lt;br /&gt;&lt;br /&gt;The S-waves (Secondary waves) are second fastest and the L-waves (Surface waves) are the last to reach the seismograph.  Though they are the slowest, the L-waves do the most damage to structures.&lt;br /&gt;&lt;br /&gt;By using the difference in arrival times between the P-waves and S-waves (as related to distance), using the difference in arrival times from three seismographs, we can triangulate to find the location of the Epicenter.&lt;br /&gt;&lt;br /&gt;S-waves do not travel through liquids, while P-waves will travel through solids and liquids.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3476154518961093160?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3476154518961093160/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3476154518961093160' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3476154518961093160'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3476154518961093160'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/few-more-noteson-earthquakes-and-stuff.html' title='A Few More Notes...on Earthquakes and stuff'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7339659971637488992</id><published>2009-05-10T22:43:00.002-04:00</published><updated>2009-05-10T23:01:26.213-04:00</updated><title type='text'>Miscellaneous stuff</title><content type='html'>&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR18jwnoI/AAAAAAAAAhU/CcxkKZyV_wk/s1600-h/Volcanics+&amp;amp;+Syncline.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334392639618850434" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 197px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR18jwnoI/AAAAAAAAAhU/CcxkKZyV_wk/s320/Volcanics+%26+Syncline.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;In the top photo are volcanics overlying a syncline.&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR1g1RepI/AAAAAAAAAhM/Rg-yiUg__oo/s1600-h/Valley+&amp;amp;+Ridge+Topography.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334392632176114322" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 201px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR1g1RepI/AAAAAAAAAhM/Rg-yiUg__oo/s320/Valley+%26+Ridge+Topography.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;In the second photo, from the Maryland Valley &amp;amp; Ridge Province, is what is called a "Water Gap", where Wills Creek (or perhaps a larger river in the past) likely cut the ridge by headward erosion.&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR1QPeDBI/AAAAAAAAAhE/4BG7_eoMcqY/s1600-h/Spanish+Peaks2.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334392627722587154" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 201px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR1QPeDBI/AAAAAAAAAhE/4BG7_eoMcqY/s320/Spanish+Peaks2.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;The third photo is of an exposed dike, showing the discordant nature of the tabular intrustion.  The mountain in the background is a small stock which represents the intrusion.  The dikes radiate outward from the stock like wagon-wheel spokes.  Because they are harder than the "country rock", they stand look like walls extending across the countryside. &lt;br /&gt;&lt;br /&gt;Don't forget, you can click on any photo to enlarge it.&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgeR1UaFgsI/AAAAAAAAAg8/IMw8R1JyB9I/s1600-h/Exfoliation+dome2.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334392628840858306" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 202px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgeR1UaFgsI/AAAAAAAAAg8/IMw8R1JyB9I/s320/Exfoliation+dome2.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;The last photo is a reminder of the exfoliation dome shape of Stone Mt..  This photo is from the old "east quarry" side of the mountain.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7339659971637488992?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7339659971637488992/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7339659971637488992' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7339659971637488992'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7339659971637488992'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/miscellaneous-stuff.html' title='Miscellaneous stuff'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeR18jwnoI/AAAAAAAAAhU/CcxkKZyV_wk/s72-c/Volcanics+%26+Syncline.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-700204630161086904</id><published>2009-05-10T22:20:00.002-04:00</published><updated>2009-05-10T22:39:15.350-04:00</updated><title type='text'>Some Sedimentary Notes</title><content type='html'>&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeMUmqdv1I/AAAAAAAAAg0/LD_J3XkY5ps/s1600-h/Well-sorted+Sediments.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334386569247571794" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeMUmqdv1I/AAAAAAAAAg0/LD_J3XkY5ps/s320/Well-sorted+Sediments.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;div&gt;The first photo shows the very well-sorted sands of a beach dune.  This is due to the actions of longshore currents and washing by wave action.&lt;br /&gt;&lt;a href="http://2.bp.blogspot.com/_h3KzFXDo8kA/SgeMUAEYfwI/AAAAAAAAAgc/hpme_6b-RO4/s1600-h/Pebbles2.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334386558887296770" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://2.bp.blogspot.com/_h3KzFXDo8kA/SgeMUAEYfwI/AAAAAAAAAgc/hpme_6b-RO4/s320/Pebbles2.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;The second photo shows poorly-sorted angular to sub-rounded pebbles in a stream gravel bar. &lt;br /&gt;&lt;/div&gt;&lt;div&gt;&lt;a href="http://3.bp.blogspot.com/_h3KzFXDo8kA/SgeMUZPcN9I/AAAAAAAAAgs/gzCF9ul46y8/s1600-h/Fissile+Shale.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334386565644564434" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://3.bp.blogspot.com/_h3KzFXDo8kA/SgeMUZPcN9I/AAAAAAAAAgs/gzCF9ul46y8/s320/Fissile+Shale.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;The third photo shows the fissile nature of shale.  Light colored shales like this were probably deposited in an open marine environment, such as a continental shelf.&lt;br /&gt;&lt;br /&gt;Red shales and siltstones are characteristic of tidal flat and delta environments.&lt;br /&gt;&lt;br /&gt;Black shales are characteristic of anoxic, oxygen-poor environments, where organics are preserved due to the lack of bacterial action.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeMUF0THRI/AAAAAAAAAgk/LG33yKHPeak/s1600-h/ChattahoocheeGravels4.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334386560430447890" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeMUF0THRI/AAAAAAAAAgk/LG33yKHPeak/s320/ChattahoocheeGravels4.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Creek and river sediments are generally poorly-sorted, such as these.  You have every size from clay to pebbles (&lt;1/256mm to 5-6 cm or more).  The contact shown is a Non-conformity, where sediments overlie igneous rock (now saprolite).&lt;br /&gt;&lt;br /&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-700204630161086904?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/700204630161086904/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=700204630161086904' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/700204630161086904'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/700204630161086904'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/some-sedimentary-notes.html' title='Some Sedimentary Notes'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_h3KzFXDo8kA/SgeMUmqdv1I/AAAAAAAAAg0/LD_J3XkY5ps/s72-c/Well-sorted+Sediments.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7567525619710273107</id><published>2009-05-10T22:02:00.003-04:00</published><updated>2009-05-10T22:20:16.838-04:00</updated><title type='text'>More Final Reviews</title><content type='html'>&lt;a href="http://3.bp.blogspot.com/_h3KzFXDo8kA/SgeKq95Op0I/AAAAAAAAAgU/DIphgXIAK90/s1600-h/FoliatedTextures.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334384754417379138" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 218px" alt="" src="http://3.bp.blogspot.com/_h3KzFXDo8kA/SgeKq95Op0I/AAAAAAAAAgU/DIphgXIAK90/s320/FoliatedTextures.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;div&gt;These photos show examples of foliated metamorphic rocks from the Ga. Piedmont and Blue Ridge.&lt;br /&gt;&lt;/div&gt;&lt;div&gt;Except for the areas immediately adjacent to diabase dikes and the largest granite bodies, the vast majority of the metamorphism in the Piedmont and Blue Ridge is &lt;strong&gt;Regional Metamorphism&lt;/strong&gt;.&lt;br /&gt;&lt;/div&gt;&lt;div&gt;Don't worry about remembering what Myllonites and Phyllonites are, the photo simply helps illustrate foliation.&lt;/div&gt;&lt;div&gt;&lt;a href="http://2.bp.blogspot.com/_h3KzFXDo8kA/SgeKCMFkhXI/AAAAAAAAAgE/9hukhaf0XGA/s1600-h/Myllonite-Phyllonite.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5334384053852603762" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://2.bp.blogspot.com/_h3KzFXDo8kA/SgeKCMFkhXI/AAAAAAAAAgE/9hukhaf0XGA/s320/Myllonite-Phyllonite.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;div&gt;&lt;/div&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7567525619710273107?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7567525619710273107/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7567525619710273107' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7567525619710273107'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7567525619710273107'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/more-final-reviews.html' title='More Final Reviews'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_h3KzFXDo8kA/SgeKq95Op0I/AAAAAAAAAgU/DIphgXIAK90/s72-c/FoliatedTextures.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7530153137695077109</id><published>2009-05-09T13:17:00.002-04:00</published><updated>2009-05-09T13:27:30.749-04:00</updated><title type='text'>Some Igneous Issues</title><content type='html'>&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgW7SjRC0lI/AAAAAAAAAfs/5nVqnZHCGbk/s1600-h/Gneiss+vs.+Granite.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5333875261068989010" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgW7SjRC0lI/AAAAAAAAAfs/5nVqnZHCGbk/s320/Gneiss+vs.+Granite.jpg" border="0" /&gt;&lt;/a&gt;The top photo shows a comparison of igneous versus metamorphic textures.&lt;br /&gt;&lt;br /&gt;Though both rocks are similar in composition, the gneiss is marked by the alignment of minerals.  The crystals in the granite are randomly oriented.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgW7TLcYnzI/AAAAAAAAAf8/ZC4k1FAh4ls/s1600-h/Phaneritic+Texture.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5333875271853973298" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgW7TLcYnzI/AAAAAAAAAf8/ZC4k1FAh4ls/s320/Phaneritic+Texture.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;div&gt;The second photo shows the most obvious difference between mafic and felsic igneous rocks.  Remember that the phaneritic, mafic rock is Gabbro, which is similar to Oceanic Crust.&lt;/div&gt;&lt;div&gt;The Granite is the phaneritic, felsic rock and is similar to the Continental Crust.  A Diorite would be a grayish color and would be a phaneritic, intermediate rock.&lt;/div&gt;&lt;div&gt; &lt;/div&gt;&lt;div&gt;Remember that the Bowen Reaction Series applies only to Silicate minerals.  The mafic minerals crystallize first, the felsic minerals last.&lt;/div&gt;&lt;div&gt; &lt;/div&gt;&lt;div&gt;More to come later...&lt;/div&gt;&lt;div&gt; &lt;/div&gt;&lt;div&gt;(Remember, you can click on each photo to enlarge it for a better look).&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7530153137695077109?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7530153137695077109/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7530153137695077109' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7530153137695077109'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7530153137695077109'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/some-igneous-issues.html' title='Some Igneous Issues'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_h3KzFXDo8kA/SgW7SjRC0lI/AAAAAAAAAfs/5nVqnZHCGbk/s72-c/Gneiss+vs.+Granite.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4342866217071734712</id><published>2009-05-09T12:41:00.003-04:00</published><updated>2009-05-09T12:49:59.816-04:00</updated><title type='text'>Erosion and Weathering and Soil</title><content type='html'>[If I repeat anything I posted earlier, please forgive.  I don't have time to go back and revisit what I previously wrote.]&lt;br /&gt;&lt;br /&gt;Remember the details about the two different types of weathering and examples&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Physical &lt;/strong&gt;- mineral chemistry doesn't change, types include ice wedging, exfoliation, root wedging.&lt;br /&gt;&lt;strong&gt;Chemical &lt;/strong&gt;- mineral chemistry changes - Hydrolysis changes feldspars and other silicates to clay, including kaolin.  Carbonic acid H2CO3 is the most common natural acid.  It comes from the mixing of rainfall and carbon dioxide.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Warm, humid conditions&lt;/strong&gt; are most favorable for chemical weathering.  Cold, dry conditions are most favorable for physical weathering.  Virtually all weathering takes place on the outcrop (rock exposure) and in the rivers on the way to the ocean.&lt;br /&gt;&lt;br /&gt;Water is the most important agent of erosion.  What water doesn't remove by erosion becomes part of the soil profile.  The "O" and "A" layers are most important to the plants.&lt;br /&gt;&lt;br /&gt;Tropical soils - &lt;strong&gt;Laterites&lt;/strong&gt;, are characterized by thin O and A layers, heavily leached subsoil.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4342866217071734712?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4342866217071734712/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4342866217071734712' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4342866217071734712'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4342866217071734712'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/erosion-and-weathering-and-soil.html' title='Erosion and Weathering and Soil'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5720499021519669501</id><published>2009-05-09T12:30:00.002-04:00</published><updated>2009-05-09T12:31:31.082-04:00</updated><title type='text'>More Notes to Come...</title><content type='html'>I was at the college a bit yesterday, but the computers in the teacher work area would not recognize my password, thus they would not let me on the internet, thus I was unable to update my website as I planned.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5720499021519669501?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5720499021519669501/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5720499021519669501' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5720499021519669501'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5720499021519669501'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/more-notes-to-come.html' title='More Notes to Come...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5568074783986786425</id><published>2009-05-07T10:52:00.003-04:00</published><updated>2009-05-07T11:00:29.998-04:00</updated><title type='text'>An Important Review Note</title><content type='html'>After having given it some thought, I decided that in the interest of time and saving gasoline, instead of going to the college today (and tomorrow), &lt;strong&gt;I will post more review notes on this blog&lt;/strong&gt; and go to the campus tomorrow, when I was already going.  It is an 88-mile round trip between here and there and with the traffic lights takes 3+ hours of driving.&lt;br /&gt;&lt;br /&gt;Besides it is easier to post new photos on my blog than the website.  The photos there (except on the Power Point) were already posted before the last format change.&lt;br /&gt;&lt;br /&gt;For your final, bring the regular Scantron.  The Assessment will use the red ones that I will furnish.&lt;br /&gt;&lt;br /&gt;So keep checking back during the day and tonight.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5568074783986786425?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5568074783986786425/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5568074783986786425' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5568074783986786425'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5568074783986786425'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/important-review-note.html' title='An Important Review Note'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5175478747160580441</id><published>2009-05-07T10:39:00.003-04:00</published><updated>2009-05-07T10:51:01.644-04:00</updated><title type='text'>More Reviews</title><content type='html'>&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgLza1SJXLI/AAAAAAAAAfk/TaOvL-0bims/s1600-h/Monitoring+wells.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5333092551065427122" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 216px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/SgLza1SJXLI/AAAAAAAAAfk/TaOvL-0bims/s320/Monitoring+wells.jpg" border="0" /&gt;&lt;/a&gt; A few water-related reviews.&lt;br /&gt;&lt;br /&gt;The monitoring wells at left show concrete &lt;strong&gt;surface pads&lt;/strong&gt;, which are the first line of defense against surface pollutants reaching the aquifer. Below the surface, &lt;strong&gt;grout in the annular space&lt;/strong&gt; is the second.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgLzanzBXQI/AAAAAAAAAfU/67f-cAA3wIY/s1600-h/Sinkhole.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5333092547445218562" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgLzanzBXQI/AAAAAAAAAfU/67f-cAA3wIY/s320/Sinkhole.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;The second photo is an example of an obvious &lt;strong&gt;losing stream&lt;/strong&gt;, which usually occurs in a karst terrane (as above) or if the water table is way below the stream bed (perhaps when a mountain stream leaves the mountains and flows into the adjacent desert).&lt;br /&gt;&lt;br /&gt;&lt;div&gt;&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgLzaorBQDI/AAAAAAAAAfc/sI430mUYEm8/s1600-h/Stream+Recovery.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5333092547680092210" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 243px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/SgLzaorBQDI/AAAAAAAAAfc/sI430mUYEm8/s320/Stream+Recovery.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;The third photo (click to enlarge) is an example of a &lt;strong&gt;gaining stream&lt;/strong&gt;, which is certainly the norm in Georgia.  The water table is&lt;strong&gt; inclined towards the stream&lt;/strong&gt;, feeding small springs and seepage to replenish the creek.&lt;br /&gt;&lt;div&gt;&lt;/div&gt;&lt;/div&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5175478747160580441?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5175478747160580441/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5175478747160580441' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5175478747160580441'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5175478747160580441'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/more-reviews.html' title='More Reviews'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_h3KzFXDo8kA/SgLza1SJXLI/AAAAAAAAAfk/TaOvL-0bims/s72-c/Monitoring+wells.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1180080978020343626</id><published>2009-05-07T09:53:00.001-04:00</published><updated>2009-05-07T09:55:17.577-04:00</updated><title type='text'>To My Lab Students</title><content type='html'>I am still working on your Lab finals and remaining papers, as well as getting ready for the lecture final (and doing my full-time job, too).&lt;br /&gt;&lt;br /&gt;Sorry for the delay, but I will know your grades on Friday.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1180080978020343626?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1180080978020343626/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1180080978020343626' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1180080978020343626'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1180080978020343626'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/to-my-lab-students.html' title='To My Lab Students'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4006071448624518162</id><published>2009-05-07T09:34:00.003-04:00</published><updated>2009-05-07T09:50:16.367-04:00</updated><title type='text'>More Review of Physical Geology Lecture Final</title><content type='html'>From the Vulcan Quarry on Beaver Ruin Road in Norcross, there are a number of things we can learn from this diabase dike having been intruded into the Lithonia Gneiss.&lt;br /&gt;&lt;a href="http://2.bp.blogspot.com/_h3KzFXDo8kA/SgLkEEd9-WI/AAAAAAAAAfE/VTBb0sgKhAA/s1600-h/Diabase+Dike+copy.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5333075667330136418" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 224px" alt="" src="http://2.bp.blogspot.com/_h3KzFXDo8kA/SgLkEEd9-WI/AAAAAAAAAfE/VTBb0sgKhAA/s320/Diabase+Dike+copy.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;*&lt;strong&gt;Cross-cutting Relationships&lt;/strong&gt; and what they tell us and who was responsible for the concept.&lt;br /&gt;*The diabase (basalt) dike is an example of a &lt;strong&gt;mafic, aphanitic igneous rock&lt;/strong&gt; in the form of a &lt;strong&gt;discordant, tabular intrusion&lt;/strong&gt;.&lt;br /&gt;*The diabase dikes are a record of the &lt;strong&gt;youngest igneous activity&lt;/strong&gt; in Georgia - during the &lt;strong&gt;Triassic and Jurassic Periods&lt;/strong&gt; (Mesozoic Era).&lt;br /&gt;*The Lithonia Gneiss was &lt;strong&gt;regionally metamorphosed&lt;/strong&gt; during one or more of the three periods of Appalachian uplift.&lt;br /&gt;*The intrusion of the diabase dike (related to the rifting of Pangea) caused a small zone of &lt;strong&gt;contact metamorphism&lt;/strong&gt; on both sides of the dike.&lt;br /&gt;*The parallel, flat breaks in the rocks are &lt;strong&gt;joints&lt;/strong&gt;, while the more irregular breaks are &lt;strong&gt;fractures&lt;/strong&gt;, (both are examples of brittle deformation).  Both joints and fractures can contribute to this rock being a &lt;strong&gt;fractured bedrock aquifer&lt;/strong&gt;.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4006071448624518162?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4006071448624518162/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4006071448624518162' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4006071448624518162'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4006071448624518162'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/more-review-of-physical-geology-lecture.html' title='More Review of Physical Geology Lecture Final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_h3KzFXDo8kA/SgLkEEd9-WI/AAAAAAAAAfE/VTBb0sgKhAA/s72-c/Diabase+Dike+copy.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5201595529893899222</id><published>2009-05-06T08:07:00.002-04:00</published><updated>2009-05-06T08:26:55.979-04:00</updated><title type='text'>Final Review Notes...</title><content type='html'>&lt;strong&gt;Because of the intense storms expected this afternoon, I will probably come to the college on Thursday to make changes to my website.  Not today.&lt;br /&gt;&lt;/strong&gt;&lt;br /&gt;I will post some study suggestions on this blog in the meantime.&lt;br /&gt;&lt;br /&gt;Beginning with...&lt;br /&gt;&lt;br /&gt;Remember the contributions of &lt;strong&gt;Nicolas Steno&lt;/strong&gt; - &lt;strong&gt;Concepts of Superposition&lt;/strong&gt;, &lt;strong&gt;Original Horizontality&lt;/strong&gt;, and &lt;strong&gt;Lateral Continuity&lt;/strong&gt;. These mainly apply to sedimentary rocks, but can apply to volcanics. Remember that you can see evidence of all three of these from the South Rim of the Grand Canyon.&lt;br /&gt;&lt;br /&gt;While on the subject of the Grand Canyon, from the same rim, you can see all three types of &lt;strong&gt;Unconformities&lt;/strong&gt; - &lt;strong&gt;Angular Unconformity&lt;/strong&gt; (between the Grand Canyon Supergroup and overlying Tonto Group; &lt;strong&gt;Disconformity&lt;/strong&gt; (between the Muav Limestone and the overlying Redwall Limestone); &lt;strong&gt;Nonconformity&lt;/strong&gt; - Tapeats Sandstone overlying the Brahma Schist.&lt;br /&gt;&lt;br /&gt;Remember that &lt;strong&gt;James Hutton&lt;/strong&gt; was responsible for concepts of &lt;strong&gt;Cross-Cutting Relationships&lt;/strong&gt; and &lt;strong&gt;Inclusions &lt;/strong&gt;- remember examples of each.&lt;br /&gt;&lt;br /&gt;More to come...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5201595529893899222?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5201595529893899222/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5201595529893899222' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5201595529893899222'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5201595529893899222'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/05/final-review-notes.html' title='Final Review Notes...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-661680138355039313</id><published>2009-04-29T11:57:00.002-04:00</published><updated>2009-04-29T12:05:00.723-04:00</updated><title type='text'>Reminders and photos</title><content type='html'>&lt;a href="http://3.bp.blogspot.com/_h3KzFXDo8kA/Sfh5ZtFaEuI/AAAAAAAAAe0/2uScKuhZVmw/s1600-h/Meander+2.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5330143641498948322" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://3.bp.blogspot.com/_h3KzFXDo8kA/Sfh5ZtFaEuI/AAAAAAAAAe0/2uScKuhZVmw/s320/Meander+2.jpg" border="0" /&gt;&lt;/a&gt; Airline photos of meandering rivers.  The pilot didn't tell us when we were over the Mississippi River.&lt;br /&gt;&lt;a href="http://1.bp.blogspot.com/_h3KzFXDo8kA/Sfh5ZYfxyAI/AAAAAAAAAes/GIohDNDdjo4/s1600-h/Meander+1.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5330143635972409346" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://1.bp.blogspot.com/_h3KzFXDo8kA/Sfh5ZYfxyAI/AAAAAAAAAes/GIohDNDdjo4/s320/Meander+1.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/Sfh5Z7ZCntI/AAAAAAAAAe8/tj9asbQDeZA/s1600-h/Meander+3.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5330143645339393746" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/Sfh5Z7ZCntI/AAAAAAAAAe8/tj9asbQDeZA/s320/Meander+3.jpg" border="0" /&gt;&lt;/a&gt; As for today's class, bring tennis shoes/boots, a water bottle, and a hat or cap - in case we have an outdoor class (or part of one).  I need to spend some time skimming over the remnants of Chapter 17, a little of Chapter 15, and...&lt;br /&gt;&lt;br /&gt;This is just the way the schedule worked out.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-661680138355039313?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/661680138355039313/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=661680138355039313' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/661680138355039313'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/661680138355039313'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/04/reminders-and-photos.html' title='Reminders and photos'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_h3KzFXDo8kA/Sfh5ZtFaEuI/AAAAAAAAAe0/2uScKuhZVmw/s72-c/Meander+2.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7369709098108153250</id><published>2009-04-20T06:23:00.008-04:00</published><updated>2009-04-20T09:38:13.636-04:00</updated><title type='text'>A Few Test Reminders...</title><content type='html'>Sorry for the delay.&lt;br /&gt;&lt;br /&gt;Remember the three types of Unconformities and where you can see all three types (ignore Paraconformities). The contact between the Cambrian Tonto Group and the Precambrian Grand Canyon Supergroup is an Angular Unconformity. The other types at the Grand Canyon are also in the Chapter 9 Power Point.&lt;br /&gt;&lt;br /&gt;Three periods of uplift for the Appalachians - 1st - &lt;strong&gt;Taconic Orogeny, Late Ordovician Period&lt;/strong&gt;; 3rd - &lt;strong&gt;Alleghenian Orogeny, Pennsylvanian Period&lt;/strong&gt; - don't concern yourself with the 2nd one as it didn't affect the Southeastern part of the continent as much.&lt;br /&gt;&lt;br /&gt;The Coastal Plain sediments are Late Mesozoic to Cenozoic and include such fossils as clams, oysters, sand dollars, and shark's teeth.&lt;br /&gt;&lt;br /&gt;Remember the characteristics of the two most common non-foliated metamorphic rocks on the Piedmont or Blue Ridge - marble and quartzite.&lt;br /&gt;&lt;br /&gt;Remember the most common green mineral - epidote.&lt;br /&gt;&lt;br /&gt;Remember the most common black crystal - tourmaline.&lt;br /&gt;&lt;br /&gt;Some important time intervals to remember - &lt;strong&gt;Cambrian Period&lt;/strong&gt; - first widespread appearance of shelled organisms; &lt;strong&gt;Pennsylvanian Period&lt;/strong&gt; - final uplift of the Appalachian Mts., large river deltas including coal swamps (and fern fossils in Ga.); &lt;strong&gt;Permian Period&lt;/strong&gt; - mass extinction of 90 - 95% of marine species; &lt;strong&gt;Triassic Period&lt;/strong&gt; - first appearance of modern corals and dinosaurs, initial rifting of Pangea (opening of the Atlantic Ocean); &lt;strong&gt;Cenozoic Era&lt;/strong&gt; - the era in which we now live; &lt;strong&gt;Quaternary Period&lt;/strong&gt; - the period in which we live; &lt;strong&gt;Holocene Epoch&lt;/strong&gt; - the epoch in which we now live.&lt;br /&gt;&lt;br /&gt;Remember what Nicolas Steno, William Smith, and James Hutton were responsible for.&lt;br /&gt;&lt;br /&gt;Remember the difference between regional metamorphism and contact metamorphism.&lt;br /&gt;&lt;br /&gt;Valley &amp;amp; Ridge fossils - brachiopods, trilobites, horn corals, crinoids, blastoids, ferns.&lt;br /&gt;&lt;br /&gt;Most of the rocks in Red Mountain (Birmingham) and Taylor Ridge (Ringgold, Ga.) are of the Red Mountain Formation - river delta and tidal flat deposits - derived from erosion of Taconic Highlands to the east.&lt;br /&gt;&lt;br /&gt;Kyanite is a bladed, blue mineral that is found in Ga.. The kyanite from Graves Mt. is short-bladed and randomly oriented in a quartzite matrix. The kyanite occurrences from Rabun and Habersham Counties are in mica schists.&lt;br /&gt;&lt;br /&gt;Remember the description of a mica schist and remember the three main types of micas that you see in Ga., Muscovite, Biotite, and Chlorite.&lt;br /&gt;&lt;br /&gt;Remember what a "Granite Pavement" ecosystem is and where is it found. Remember what the solution pits are and the unusual plants that grow in them at Mt. Arabia.&lt;br /&gt;&lt;br /&gt;Remember the types of aquifers for the Ga. Provinces.&lt;br /&gt;&lt;br /&gt;Remember that the dinosaurs became extinct at the end of the Cretaceous Period.&lt;br /&gt;&lt;br /&gt;Remember what causes "snowball garnets" (shearing of a schist during metamorphism) and that snowball garnets would probably not show any good crystal faces, unless the shearing stopped before the crystal finished growing.&lt;br /&gt;&lt;br /&gt;Most garnets come from metamorphic rocks.&lt;br /&gt;&lt;br /&gt;Museum-quality rutile crystals come from Graves Mt., in Lincoln County.&lt;br /&gt;&lt;br /&gt;In a broad definition of the Appalachians, the Valley &amp;amp; Ridge, Blue Ridge, and Piedmont are all included.&lt;br /&gt;&lt;br /&gt;Remember the Fall Line cities in Ga..&lt;br /&gt;&lt;br /&gt;More to come...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7369709098108153250?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7369709098108153250/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7369709098108153250' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7369709098108153250'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7369709098108153250'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/04/few-test-reminders.html' title='A Few Test Reminders...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3197794906793268550</id><published>2009-04-11T23:13:00.003-04:00</published><updated>2009-04-11T23:16:00.224-04:00</updated><title type='text'>About the odd shaped piece of quartzite...</title><content type='html'>(I don't have a photo to remind you, but it was sample #28).&lt;br /&gt;&lt;br /&gt;It has its particular shape because it was part of a fold.  It was probably surrounded by mica schist that weathered away, leaving the quartzite behind.&lt;br /&gt;&lt;br /&gt;Remember, at the surface, quartz and quartzite are relatively stable and do not undergo chemical weathering.&lt;br /&gt;&lt;br /&gt;We will do a little more of the "Ga. stuff" on Monday, then have Exam III on Wednesday.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3197794906793268550?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3197794906793268550/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3197794906793268550' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3197794906793268550'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3197794906793268550'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/04/about-odd-shaped-piece-of-quartzite.html' title='About the odd shaped piece of quartzite...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6088636762967951100</id><published>2009-04-01T10:05:00.003-04:00</published><updated>2009-04-01T10:08:23.604-04:00</updated><title type='text'>Announcements for Wednesday, April 1 - No Foolin'</title><content type='html'>I decided not to have the test today.  (Honestly).&lt;br /&gt;&lt;br /&gt;Instead, we will "break into" small groups to work on an in-class project, which will familiarize you a little more with Georgia, metamorphics, and geologic time.&lt;br /&gt;&lt;br /&gt;If it is not too much of an inconvenience, is it possible for any students to bring their lab manual, so there is at least one in each group?  They might be useful for looking up some mineral info.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6088636762967951100?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6088636762967951100/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6088636762967951100' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6088636762967951100'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6088636762967951100'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/04/announcements-for-wednesday-april-1-no.html' title='Announcements for Wednesday, April 1 - No Foolin&apos;'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1898960477234663522</id><published>2009-03-30T10:29:00.002-04:00</published><updated>2009-03-30T10:31:54.295-04:00</updated><title type='text'>Announcements for Monday, March 30, 2009</title><content type='html'>As it is still too wet to go outside for class (maybe Wednesday), today in lecture we will review Chapters 8 &amp;amp; 9 and Georgia Geology Notes.  If the weather is nice on Wednesday, we may have class outside.  If has rained again, we will have Exam III.&lt;br /&gt;&lt;br /&gt;In lab, we are going to do Lab 9, on maps.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1898960477234663522?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1898960477234663522/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1898960477234663522' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1898960477234663522'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1898960477234663522'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/03/announcements-for-monday-march-30-2009.html' title='Announcements for Monday, March 30, 2009'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-991180796356455948</id><published>2009-03-23T12:21:00.003-04:00</published><updated>2009-03-23T12:23:40.599-04:00</updated><title type='text'>Announcements for Monday March 23</title><content type='html'>For Lab, there will be an open-book "mid-term" exam.&lt;br /&gt;&lt;br /&gt;For lecture, if you haven't yet printed out the "Georgia Geology Notes Part I or Part II", don't do so, as I redid that Power Point this morning and will upload it when I get to the campus, a little later.&lt;br /&gt;&lt;br /&gt;BTW, Redoubt Volcano &lt;a href="http://www.avo.alaska.edu/activity/Redoubt.php"&gt;is busy&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;Sorry for the late notice on the exam and Power Point.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-991180796356455948?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/991180796356455948/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=991180796356455948' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/991180796356455948'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/991180796356455948'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/03/announcements-for-monday-march-23.html' title='Announcements for Monday March 23'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-815048593820913168</id><published>2009-03-16T13:26:00.002-04:00</published><updated>2009-03-16T13:35:56.034-04:00</updated><title type='text'>Class Update</title><content type='html'>&lt;a href="http://4.bp.blogspot.com/_h3KzFXDo8kA/Sb6MYyyMzvI/AAAAAAAAAeM/vVRoxmSuPM8/s1600-h/Ben+2.JPG"&gt;&lt;img id="BLOGGER_PHOTO_ID_5313838967920840434" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://4.bp.blogspot.com/_h3KzFXDo8kA/Sb6MYyyMzvI/AAAAAAAAAeM/vVRoxmSuPM8/s320/Ben+2.JPG" border="0" /&gt;&lt;/a&gt; To my classes;&lt;br /&gt;&lt;br /&gt;Sorry that I hadn't posted any news here during Spring Break.  Our daughter gave birth to our first grandchild, a grandson last Tuesday.  So we have been busy with that special event.&lt;br /&gt;&lt;br /&gt;As for the exam, I have been wrestling with how to grade these, as I made them longer than I should have and didn't get the chance to review as I wanted to because of the snow day.&lt;br /&gt;&lt;br /&gt;We will be doing the Chapter on Metamorphic rocks this afternoon and Wednesday.&lt;br /&gt;&lt;br /&gt;See you this afternoon.&lt;br /&gt;&lt;br /&gt;Remember the April 18th field trip, there still may be a few openings.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://2.bp.blogspot.com/_h3KzFXDo8kA/Sb6MYYyYRYI/AAAAAAAAAeE/VJFEM7dHJeE/s1600-h/Ben+3.JPG"&gt;&lt;img id="BLOGGER_PHOTO_ID_5313838960942269826" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://2.bp.blogspot.com/_h3KzFXDo8kA/Sb6MYYyYRYI/AAAAAAAAAeE/VJFEM7dHJeE/s320/Ben+3.JPG" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;div&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-815048593820913168?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/815048593820913168/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=815048593820913168' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/815048593820913168'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/815048593820913168'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/03/class-update.html' title='Class Update'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_h3KzFXDo8kA/Sb6MYyyMzvI/AAAAAAAAAeM/vVRoxmSuPM8/s72-c/Ben+2.JPG' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5713029466874837783</id><published>2009-03-02T14:17:00.002-05:00</published><updated>2009-03-02T14:21:43.886-05:00</updated><title type='text'>Just a Reminder</title><content type='html'>If you didn't get the word, there is no class tonight, due to the re-icing of snow and slush.&lt;br /&gt;&lt;br /&gt;I do need you to send me a notice if you want to go on the April 18th field trip to NW Ga.  It is only $5, but you will need to bring lunch and a water bottle and plan to be gone most of the day.&lt;br /&gt;&lt;br /&gt;For Lab only students, have a nice spring break.  For lecture, I will have to figure out something, 'cause until an hour ago, I thought we had class.  Bring books and notes - in case I decide to have an open book test.  Or we might just go with what we have for a regular test, as we only had two chapters.  Go back and reread the Power Point notes.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5713029466874837783?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5713029466874837783/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5713029466874837783' title='1 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5713029466874837783'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5713029466874837783'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/03/just-reminder.html' title='Just a Reminder'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3312743748098750784</id><published>2009-02-24T23:12:00.002-05:00</published><updated>2009-02-24T23:17:03.346-05:00</updated><title type='text'>GPC Sponsored Field Trip - April 18</title><content type='html'>Just a reminder, there is a field trip sponsored by GPC to the Valley &amp;amp; Ridge Province of Georgia.  We haven't yet gotten into the Geologic Provinces of Ga. yet, but the Valley &amp;amp; Ridge is the area between Cartersville, GA and Chattanooga, TN.&lt;br /&gt;&lt;br /&gt;The area is characterized by folded and faulted, old sedimentary rocks, some with fossils.&lt;br /&gt;&lt;br /&gt;The bus trip is $5 and you need to bring a sack lunch and a water bottle.  There will be numerous stops, some of them may be on private land, which we might not be able to visit if not for the permission gained for this trip.&lt;br /&gt;&lt;br /&gt;Let me know if you are interested.  It will take most of the day and I think they are leaving from the Clarkston campus.  Will get back to you with more details.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3312743748098750784?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3312743748098750784/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3312743748098750784' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3312743748098750784'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3312743748098750784'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/02/gpc-sponsored-field-trip-april-18.html' title='GPC Sponsored Field Trip - April 18'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7917322519690184631</id><published>2009-02-18T06:20:00.002-05:00</published><updated>2009-02-18T06:23:38.870-05:00</updated><title type='text'>For Today's Exam</title><content type='html'>If you weren't in class on Monday, email me ASAP at jsummerour@hotmail.com so I can send you one of the Study Guides.  You need to fill it out and then you can use it as a note sheet for the test.&lt;br /&gt;&lt;br /&gt;For those of you with the Study Guides, just a reminder, there is a typo on the right column.  "R" should be Porphyritic Texture, not Phaneritic.&lt;br /&gt;&lt;br /&gt;The link for the next Chapter doesn't work, yet, but it should by the time of the test.&lt;br /&gt;&lt;br /&gt;Good Luck.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7917322519690184631?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7917322519690184631/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7917322519690184631' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7917322519690184631'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7917322519690184631'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/02/for-todays-exam.html' title='For Today&apos;s Exam'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2574514217567776233</id><published>2009-01-19T11:15:00.002-05:00</published><updated>2009-01-19T11:17:32.881-05:00</updated><title type='text'>For Later in the Semester...</title><content type='html'>when we cover "Mass Wasting", here is a &lt;a href="http://geology.com/articles/yosemite-rockfall.shtml"&gt;sequence of photos&lt;/a&gt; of a Rock Fall and Rock Slide in Yosemite National Park, last year.&lt;br /&gt;&lt;br /&gt;Fortunately, there were no campers/rock climbers below the event.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2574514217567776233?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2574514217567776233/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2574514217567776233' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2574514217567776233'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2574514217567776233'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/01/for-later-in-semester.html' title='For Later in the Semester...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-477846890144569553</id><published>2009-01-14T11:22:00.007-05:00</published><updated>2009-01-14T12:19:50.109-05:00</updated><title type='text'>Yellowstone Caldera (Supervolcano)</title><content type='html'>&lt;a href="http://2.bp.blogspot.com/_h3KzFXDo8kA/SW4W824i_XI/AAAAAAAAAbs/0udNQHSSZzs/s1600-h/Earthquake+index.gif"&gt;&lt;img style="float:left; margin:0 10px 10px 0;cursor:pointer; cursor:hand;width: 261px; height: 320px;" src="http://2.bp.blogspot.com/_h3KzFXDo8kA/SW4W824i_XI/AAAAAAAAAbs/0udNQHSSZzs/s320/Earthquake+index.gif" border="0" alt=""id="BLOGGER_PHOTO_ID_5291191846987562354" /&gt;&lt;/a&gt;&lt;br /&gt;Per a student request, here are a couple of Supervolcano videos and an index map showing &lt;a href="http://earthquake.usgs.gov/eqcenter/recenteqsus/"&gt;recent earthquake activity&lt;/a&gt;, &lt;a href="http://earthquake.usgs.gov/eqcenter/recenteqsus/Maps/special/Yellowstone.php"&gt;including Yellowstone earthquake activity&lt;/a&gt; and &lt;a href="http://folkworm.ceri.memphis.edu/recenteqs/"&gt;southeastern US&lt;/a&gt;:&lt;br /&gt;&lt;br /&gt;&lt;embed src="http://www.youtube.com/v/zh9zVXUv-Fs&amp;amp;hl=" fs="1" width="425" height="344" type="application/x-shockwave-flash" allowfullscreen="true" allowscriptaccess="always"&gt;&lt;/embed&gt;&lt;br /&gt;&lt;br /&gt;The first one from shortskivt and First Science TV&lt;br /&gt;&lt;br /&gt;The second one is from Sustainable Angels:&lt;br /&gt;&lt;br /&gt;&lt;embed src="http://www.youtube.com/v/JmFWfmzOoi0&amp;amp;hl=" fs="1" width="425" height="344" type="application/x-shockwave-flash" allowfullscreen="true" allowscriptaccess="always"&gt;&lt;/embed&gt;&lt;br /&gt;&lt;br /&gt;After watching part of the second video, this guy's geological information, timescales, and cause/effect relationships &lt;strong&gt;&lt;span style="font-size:130%;"&gt;are all screwed up&lt;/span&gt;&lt;/strong&gt;. It is an interesting video, some good images, just take the prior history and causes with a shaker of salt.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-477846890144569553?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/477846890144569553/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=477846890144569553' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/477846890144569553'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/477846890144569553'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2009/01/yellowstone-caldera-supervolcano.html' title='Yellowstone Caldera (Supervolcano)'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_h3KzFXDo8kA/SW4W824i_XI/AAAAAAAAAbs/0udNQHSSZzs/s72-c/Earthquake+index.gif' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5449821406997400627</id><published>2008-12-10T08:36:00.000-05:00</published><updated>2008-12-10T06:05:32.807-05:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Geology Videos'/><title type='text'>Geology Videos - #1</title><content type='html'>Rock identification, from a former Marine's video.  Originated by "devildogmre", he is now a student at East Tennessee State University.  The commentary seems to be him and another student:&lt;br /&gt;&lt;br /&gt;&lt;object width="425" height="344"&gt;&lt;param name="movie" value="http://www.youtube.com/v/3vgNvXdkQaU&amp;hl=en&amp;fs=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/3vgNvXdkQaU&amp;hl=en&amp;fs=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="425" height="344"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;Not totally scientific, but you might remember some of the identifications.&lt;br /&gt;&lt;br /&gt;The second video, from "Studio4Learning"&lt;br /&gt;&lt;br /&gt;&lt;object width="425" height="344"&gt;&lt;param name="movie" value="http://www.youtube.com/v/TuOIDg41MZE&amp;hl=en&amp;fs=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/TuOIDg41MZE&amp;hl=en&amp;fs=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="425" height="344"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;Probably for a high-school class, a short video, but still provides some information.&lt;br /&gt;&lt;br /&gt;Another video, a follow-up from "Studio4Learning":&lt;br /&gt;&lt;br /&gt;&lt;object width="425" height="344"&gt;&lt;param name="movie" value="http://www.youtube.com/v/Frjjh7F3kuc&amp;hl=en&amp;fs=1"&gt;&lt;/param&gt;&lt;param name="allowFullScreen" value="true"&gt;&lt;/param&gt;&lt;param name="allowscriptaccess" value="always"&gt;&lt;/param&gt;&lt;embed src="http://www.youtube.com/v/Frjjh7F3kuc&amp;hl=en&amp;fs=1" type="application/x-shockwave-flash" allowscriptaccess="always" allowfullscreen="true" width="425" height="344"&gt;&lt;/embed&gt;&lt;/object&gt;&lt;br /&gt;&lt;br /&gt;Hope you find these informative and entertaining.&lt;br /&gt;&lt;br /&gt;[I would have posted videos earlier, but I didn't learn how to do this until yesterday (12/09/08).]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5449821406997400627?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5449821406997400627/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5449821406997400627' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5449821406997400627'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5449821406997400627'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/12/geology-videos-1.html' title='Geology Videos - #1'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-8744085845540473007</id><published>2008-12-10T08:32:00.000-05:00</published><updated>2008-12-10T06:06:06.858-05:00</updated><title type='text'>To All Classes...</title><content type='html'>I apologize for not having posted more finals-related info here.  As you know, I had been coughing quite a bit lately because of a sinus infection.  It turned into bronchitis and I have just been too sick the last few days to get much done.  I am getting better, but it takes time.&lt;br /&gt;&lt;br /&gt;I would ask that you keep checking here, in the name of your continuing science education, as I will be posting YouTube videos on science issues, after I screen them.&lt;br /&gt;&lt;br /&gt;Good Luck with your finals and your future.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-8744085845540473007?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/8744085845540473007/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=8744085845540473007' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8744085845540473007'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8744085845540473007'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/12/to-all-classes.html' title='To All Classes...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3740156383373184891</id><published>2008-12-08T11:28:00.000-05:00</published><updated>2008-12-08T11:31:33.122-05:00</updated><title type='text'>To My Physical Geology Class...</title><content type='html'>I will try to post some study tips later. I have been sick with a sinus infection and bronchitis. I was going to come to the college today to update my website, but I am too sick to drive that far.&lt;br /&gt;&lt;br /&gt;My apologies.&lt;br /&gt;&lt;br /&gt;P.S.; The final is at 1 PM, not 1:45 PM on Wednesday.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3740156383373184891?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3740156383373184891/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3740156383373184891' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3740156383373184891'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3740156383373184891'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/12/to-my-physical-geology-class.html' title='To My Physical Geology Class...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6997722256874571990</id><published>2008-12-01T21:39:00.000-05:00</published><updated>2008-12-01T21:41:53.011-05:00</updated><title type='text'>Geology Class - Exam IV Reminders</title><content type='html'>The exam is most likely to be an open-book/open-note exam on Chapters 15 (Mass Wasting), Chapter 16 (Running Water), Chapter 17 (Groundwater) and Chapter 20 (Shoreline Processes).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6997722256874571990?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6997722256874571990/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6997722256874571990' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6997722256874571990'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6997722256874571990'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/12/geology-class-exam-iv-reminders.html' title='Geology Class - Exam IV Reminders'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2769826479050043893</id><published>2008-11-29T00:09:00.001-05:00</published><updated>2008-11-29T00:09:53.890-05:00</updated><title type='text'>Physical Geology Chapter 20 Info</title><content type='html'>Here is a link to a website on Beach issues.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.uky.edu/AS/Geology/howell/goodies/elearning/module14swf.swf"&gt;http://www.uky.edu/AS/Geology/howell/goodies/elearning/module14swf.swf&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2769826479050043893?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2769826479050043893/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2769826479050043893' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2769826479050043893'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2769826479050043893'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/physical-geology-chapter-20-info.html' title='Physical Geology Chapter 20 Info'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1777809624223137733</id><published>2008-11-20T11:37:00.001-05:00</published><updated>2008-11-20T11:37:31.736-05:00</updated><title type='text'>Newton County Recycling Info</title><content type='html'>&lt;a href="http://co.newton.ga.us/content/view/19/31/"&gt;http://co.newton.ga.us/content/view/19/31/&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1777809624223137733?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1777809624223137733/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1777809624223137733' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1777809624223137733'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1777809624223137733'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/newton-county-recycling-info.html' title='Newton County Recycling Info'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5865148132356151296</id><published>2008-11-19T22:43:00.000-05:00</published><updated>2008-11-19T22:45:38.611-05:00</updated><title type='text'>For Thursday, November 20th</title><content type='html'>We will spend the first 15 minutes or so of class reviewing the "Review Sheets" that you were given on Tuesday, then we will do the retest.&lt;br /&gt;&lt;br /&gt;I changed my mind, we will not be using the Review Sheet during the test.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5865148132356151296?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5865148132356151296/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5865148132356151296' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5865148132356151296'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5865148132356151296'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/for-thursday-november-20th.html' title='For Thursday, November 20th'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-213388750524844513</id><published>2008-11-18T17:07:00.000-05:00</published><updated>2008-11-18T17:13:23.444-05:00</updated><title type='text'>Environmental Science Re-test Review Answers</title><content type='html'>There will be a re-test of Exam III (a shorter version on Thursday).  If you missed today's class, email me at my hotmail address and I will send you an attached copy of the homework.  You need to fill in the homework and study it for this is the source of the questions for Thursday.&lt;br /&gt;&lt;br /&gt;In order:&lt;br /&gt;&lt;br /&gt;Q - Winds uplifted...&lt;br /&gt;W&lt;br /&gt;J&lt;br /&gt;T&lt;br /&gt;X&lt;br /&gt;A&lt;br /&gt;O - Clockwise circulation,...&lt;br /&gt;C&lt;br /&gt;AA&lt;br /&gt;L&lt;br /&gt;DD&lt;br /&gt;Z&lt;br /&gt;B&lt;br /&gt;F&lt;br /&gt;D - Inhibits nutrient...&lt;br /&gt;CC&lt;br /&gt;EE&lt;br /&gt;E&lt;br /&gt;G&lt;br /&gt;I&lt;br /&gt;H&lt;br /&gt;K&lt;br /&gt;M - Terms to describe...&lt;br /&gt;N&lt;br /&gt;P&lt;br /&gt;BB&lt;br /&gt;R&lt;br /&gt;S&lt;br /&gt;U&lt;br /&gt;V&lt;br /&gt;Y - Causes waves in...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-213388750524844513?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/213388750524844513/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=213388750524844513' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/213388750524844513'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/213388750524844513'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/environmental-science-re-test-review.html' title='Environmental Science Re-test Review Answers'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-8986918748182711603</id><published>2008-11-18T12:06:00.000-05:00</published><updated>2008-11-18T12:13:50.352-05:00</updated><title type='text'>Idiot Alert!</title><content type='html'>Restrictions on car-pooling in Ontario, Canada.  A privately-owned startup firm helps put people together for the purpose of carpooling on an as-needed basis.  A bus company threw a fit and sued because they weren't following the laws as decreed by the government.&lt;br /&gt;&lt;br /&gt;From the article:&lt;br /&gt;&lt;br /&gt;&lt;em&gt;..."The only way you can ride with someone is if you meet ALL of the following extremely impractical set of specific criteria:&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;&lt;em&gt;* You must travel from home to work only – (Not Home to School, or Home to the Hospital or the Airport)&lt;/em&gt;&lt;br /&gt;&lt;em&gt;* You cannot cross municipal boundaries – (Live outside the city and drive in – sorry you cannot share the ride with your neighbour)&lt;/em&gt;&lt;br /&gt;&lt;em&gt;* You must ride with the same driver each day – (Want to mix it up go with one person one day and another person another day – no sorry cannot do that – must be same person each day)&lt;/em&gt;&lt;br /&gt;&lt;em&gt;* You must pay the driver no more frequently than weekly – (Neighbour drives you to work better not pay her right away just in case she drives you later on in the week)"...&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;Read the story &lt;a href="http://www.techcrunch.com/2008/11/12/ill-never-let-canada-live-this-down/"&gt;here&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.youtube.com/watch?v=66N6ifAFrFs&amp;amp;feature=related"&gt;Blame Canada!&lt;/a&gt;  (Just kidding, I have relatives in British Columbia).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-8986918748182711603?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/8986918748182711603/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=8986918748182711603' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8986918748182711603'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8986918748182711603'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/idiot-alert.html' title='Idiot Alert!'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3608327400717367440</id><published>2008-11-11T08:45:00.000-05:00</published><updated>2008-11-11T08:46:52.942-05:00</updated><title type='text'>For the Physical Geology class ONLY!</title><content type='html'>Today's Exam III will be open-book/open-note, so bring your stuff and your regular Scantrons.&lt;br /&gt;&lt;br /&gt;Sorry for the late decision, I decided that we hadn't covered the material enough for the number of chapters that are on this test.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3608327400717367440?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3608327400717367440/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3608327400717367440' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3608327400717367440'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3608327400717367440'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/for-physical-geology-class-only.html' title='For the Physical Geology class ONLY!'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6993755929208412144</id><published>2008-11-10T09:41:00.000-05:00</published><updated>2008-11-10T08:27:43.792-05:00</updated><title type='text'>For Environmental Science Class</title><content type='html'>This in-class assignment will probably be next Tuesday 10/28 - on the Temperate Deciduous Forest biome. Don't worry about Exam III for the near-term. It is important that we learn more about our own biome/ecosystem.&lt;br /&gt;&lt;br /&gt;Here are a few websites on this subject.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.enchantedlearning.com/biomes/tempdecid/tempdecid.shtml"&gt;Enchanted Learning&lt;/a&gt;. &lt;a href="http://www.fw.vt.edu/dendro/Forsite/tdfbiome.htm"&gt;Univ. of Vermont&lt;/a&gt;. &lt;a href="http://www.nhptv.org/natureworks/nwep8c.htm"&gt;Nature Works&lt;/a&gt;. &lt;a href="http://www.mbgnet.net/sets/temp/whats.htm"&gt;MBGNET&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;This is important as this is our biome.&lt;/strong&gt; Spend some more time on these websites. Remember examples from each of the five layers of vegetation from the Enchanted Learning website.&lt;br /&gt;&lt;br /&gt;Another name for the "Tree Stratum" is "Canopy Trees", for the biggest hardwoods (or pines in a younger forest).&lt;br /&gt;&lt;br /&gt;[A little more later today, check back.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6993755929208412144?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6993755929208412144/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6993755929208412144' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6993755929208412144'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6993755929208412144'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/10/for-environmental-science-class.html' title='For Environmental Science Class'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7940594444571696097</id><published>2008-11-06T07:02:00.000-05:00</published><updated>2008-11-06T07:04:12.088-05:00</updated><title type='text'>Recycling Expo</title><content type='html'>There is going to be a three-day Recycling Expo on the third floor - Nov. 11 -13.&lt;br /&gt;&lt;br /&gt;I will hand out a question sheet for you to fill in as a homework assignment.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7940594444571696097?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7940594444571696097/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7940594444571696097' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7940594444571696097'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7940594444571696097'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/recycling-expo.html' title='Recycling Expo'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1830778204660426878</id><published>2008-11-06T05:43:00.000-05:00</published><updated>2008-11-06T05:52:01.982-05:00</updated><title type='text'>Geology Class</title><content type='html'>We will not have Chapter 15 - Mass Wasting on Exam III.  I will emphasize the other important material today.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1830778204660426878?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1830778204660426878/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1830778204660426878' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1830778204660426878'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1830778204660426878'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/11/geology-class.html' title='Geology Class'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4964114147640555294</id><published>2008-10-28T13:46:00.001-04:00</published><updated>2008-10-28T13:54:47.178-04:00</updated><title type='text'>Thursday, Oct. 30th Classes</title><content type='html'>Bring your outdoor shoes, in case the weather is suitable for an outdoor class.&lt;br /&gt;&lt;br /&gt;For all classes, here are some map links.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://georgiainfo.galileo.usg.edu/physiographic/physio-dist.htm"&gt;Georgia Physiographic Provinces&lt;/a&gt;.  Click on some of the regions, e.g., the Washington Slope and the Winder Slope for an explanation.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://coastgis.marsci.uga.edu/summit/whatbasin.htm"&gt;Georgia River Basins&lt;/a&gt;. &lt;br /&gt;&lt;br /&gt;&lt;a href="http://georgiainfo.galileo.usg.edu/pdf/gacount3.pdf"&gt;Georgia Counties&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.georgiaplanning.com/watertoolkit/Documents/PublicationEducationInvolvement/KABAffiliatesandGeorgiaWatershedsMap.pdf"&gt;Georgia Watersheds&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;More may be added.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4964114147640555294?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4964114147640555294/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4964114147640555294' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4964114147640555294'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4964114147640555294'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/10/thursday-oct-30th-classes.html' title='Thursday, Oct. 30th Classes'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3308642135016907793</id><published>2008-10-06T21:44:00.001-04:00</published><updated>2008-10-06T21:47:49.557-04:00</updated><title type='text'>A Comparison of Oceanic and Continental Crust Material</title><content type='html'>&lt;a href="http://3.bp.blogspot.com/_h3KzFXDo8kA/SOq_hwfbezI/AAAAAAAAAQc/_mNrync2Ifw/s1600-h/Phaneritic+Texture.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5254222501954419506" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; CURSOR: hand" alt="" src="http://3.bp.blogspot.com/_h3KzFXDo8kA/SOq_hwfbezI/AAAAAAAAAQc/_mNrync2Ifw/s320/Phaneritic+Texture.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;div&gt;&lt;/div&gt;&lt;br /&gt;The Gabbro on the Left is similar to Oceanic Crust, while the Granite on the Right is similar to Continental Crust.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3308642135016907793?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3308642135016907793/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3308642135016907793' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3308642135016907793'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3308642135016907793'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/10/comparison-of-oceanic-and-continental.html' title='A Comparison of Oceanic and Continental Crust Material'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_h3KzFXDo8kA/SOq_hwfbezI/AAAAAAAAAQc/_mNrync2Ifw/s72-c/Phaneritic+Texture.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6214111093203869110</id><published>2008-09-11T18:40:00.000-04:00</published><updated>2008-09-14T15:23:36.997-04:00</updated><title type='text'>Gulf of Mexico info</title><content type='html'>The two most important things to read are:&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;1) &lt;/span&gt;&lt;/strong&gt;&lt;a href="http://gulfmex.org/facts.htm"&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;Gulf of Mexico facts and threats&lt;/span&gt;&lt;/strong&gt;&lt;/a&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;. &lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;2) &lt;/span&gt;&lt;/strong&gt;&lt;a href="http://www.reason.com/news/printer/34781.html"&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;Artificial Reefs&lt;/span&gt;&lt;/strong&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Other stuff that might help you understand the subject a little better:&lt;br /&gt;&lt;a href="http://gulfmex.org/map.htm"&gt;Gulf of Mexico maps&lt;/a&gt; , &lt;a href="http://flowergarden.noaa.gov/"&gt;Flower Garden Banks Reef&lt;/a&gt;, &lt;a href="http://www.artificialreefs.org/"&gt;Reef Balls&lt;/a&gt;, &lt;a href="http://www.reefmaker.com/"&gt;ReefMakers&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;Try this! "&lt;a href="http://www.nhc.noaa.gov/HAW2/english/kids/movncane.swf"&gt;Aim a Hurricane&lt;/a&gt;" sent to me by one of your classmates. By putting the Low Pressure and High Pressure Systems in different locations, you can see how this affects the track of a hurricane.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6214111093203869110?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6214111093203869110/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6214111093203869110' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6214111093203869110'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6214111093203869110'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/09/gulf-of-mexico-info.html' title='Gulf of Mexico info'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1190724039196289793</id><published>2008-08-19T07:59:00.000-04:00</published><updated>2008-08-19T08:03:26.036-04:00</updated><title type='text'>Global Warming...How it All Began</title><content type='html'>Prior to 1980, the Hypothesis that Anthropogenic (Human caused) carbon dioxide could cause significant global warming was obscure.&lt;br /&gt;&lt;br /&gt;Read &lt;a href="http://www.john-daly.com/history.htm"&gt;this article&lt;/a&gt; to find out how and why government got involved.  And what happens after that.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1190724039196289793?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1190724039196289793/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1190724039196289793' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1190724039196289793'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1190724039196289793'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/08/global-warminghow-it-all-began.html' title='Global Warming...How it All Began'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-9187090620957595870</id><published>2008-07-28T08:54:00.000-04:00</published><updated>2008-07-28T09:21:20.759-04:00</updated><title type='text'>Late Exam Reminders...</title><content type='html'>Sorry for the delays.  Have been pre-occupied with mechanical repairs to both family cars and my digital camera, as well as grading Exam IV and the Lab Final.&lt;br /&gt;&lt;br /&gt;A few things to review:&lt;br /&gt;&lt;br /&gt;Some of the synonyms -&lt;br /&gt;&lt;br /&gt;Subduction Zone/Convergent Zone&lt;br /&gt;Rift Zone/Divergent Zone&lt;br /&gt;Stratovolcano/Composite Volcano&lt;br /&gt;Basalt/Diabase&lt;br /&gt;Stagnant/Anoxic/Anaerobic/Oxygen-Poor/Reducing Environment&lt;br /&gt;&lt;br /&gt;Other stuff -&lt;br /&gt;&lt;br /&gt;If I mention the GUC campus, instead of GPC Covington, the same applies as they are both on the Piedmont.&lt;br /&gt;&lt;br /&gt;In some limestones and shales, the dark color is because of the presence of organic matter and suggests deposition in an anoxic (oxygen-poor environment).&lt;br /&gt;&lt;br /&gt;A flooded stream's Capacity (the quantity of transported load) is related to its discharge.  The discharge is a measure of the volume of water passing a given point.&lt;br /&gt;&lt;br /&gt;Non-foliated metamorphic rocks - primarily quartzite and marble.&lt;br /&gt;&lt;br /&gt;A rock dominated by small, aligned mica flakes (that you can see) is a mica schist.&lt;br /&gt;&lt;br /&gt;Muscovite mica - light brown.  Biotite mica - black.&lt;br /&gt;&lt;br /&gt;Quartz - no cleavage, irregular to concoidinal (curving) fracture.&lt;br /&gt;&lt;br /&gt;Potassium Feldspar - 2 directions of cleavage at 90 degrees to each other.&lt;br /&gt;&lt;br /&gt;Most of the Piedmont rocks are regionally metamorphosed.&lt;br /&gt;&lt;br /&gt;Remember what an Angular Unconformity is and that the Cambrian Tonto Group in the Grand Canyon is deposited over an Angular Unconformity.&lt;br /&gt;&lt;br /&gt;Most of the igneous rocks (granite, diabase) in Georgia are on the Piedmont.  The high mountain peaks and marble are in the Blue Ridge.&lt;br /&gt;&lt;br /&gt;The Bowen Reaction Series applies only to Silicate Minerals.&lt;br /&gt;&lt;br /&gt;A Base Level rise triggers deposition.  A Base Level fall triggers erosion. &lt;br /&gt;&lt;br /&gt;Building a dam raises Base Level upstream.  Tearing down a dam lowers Base Level upstream.&lt;br /&gt;&lt;br /&gt;[Will try to add more.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-9187090620957595870?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/9187090620957595870/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=9187090620957595870' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/9187090620957595870'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/9187090620957595870'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/07/late-exam-reminders.html' title='Late Exam Reminders...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1446887739790719140</id><published>2008-07-23T18:29:00.000-04:00</published><updated>2008-07-23T18:59:08.972-04:00</updated><title type='text'>A Few Tips for the Lab Final</title><content type='html'>For Lab 9, on Topographic Maps, review the Table on page 174 - "Rules for Contour Lines". Especially remember the "Law of "vees"", when contour lines cross a stream, the "vee" always points upstream.&lt;br /&gt;&lt;br /&gt;Also remember that concentric closed contours represent a hill and that enclosed contour lines, with inward-pointing hatchure marks indicate an enclosed depression.&lt;br /&gt;&lt;br /&gt;Remember what Index contours are and how to determine the contour interval.&lt;br /&gt;&lt;br /&gt;On page 189, remember how to do a topographic profile and how to visualize a profile along a line across a topo map.&lt;br /&gt;&lt;br /&gt;On Lab 10, remember the symbols for Strike &amp;amp; Dip and other symbols for anticlines, synclines, plunging anticlines, etc..&lt;br /&gt;&lt;br /&gt;[More will be added a little later. Keep studying the two exams that I gave back to you.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1446887739790719140?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1446887739790719140/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1446887739790719140' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1446887739790719140'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1446887739790719140'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/07/few-tips-for-lab-final.html' title='A Few Tips for the Lab Final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6750591672217805580</id><published>2008-07-17T13:13:00.001-04:00</published><updated>2008-07-17T14:06:09.114-04:00</updated><title type='text'>Links for Exam IV</title><content type='html'>In case I don't get the time to update my website, here are some links.&lt;br /&gt;&lt;br /&gt;Gwinnett County info  &lt;a href="http://www.gwinnettcounty.com/cgi-bin/gwincty/egov/ep/gcbrowse.do?channelId=-49520&amp;amp;pageTypeId=536880236"&gt;http://www.gwinnettcounty.com/cgi-bin/gwincty/egov/ep/gcbrowse.do?channelId=-49520&amp;amp;pageTypeId=536880236&lt;/a&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6750591672217805580?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6750591672217805580/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6750591672217805580' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6750591672217805580'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6750591672217805580'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/07/links-for-exam-iv.html' title='Links for Exam IV'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2009584220242349548</id><published>2008-06-26T19:43:00.000-04:00</published><updated>2008-06-26T19:45:54.778-04:00</updated><title type='text'>Sorry for Missing Class</title><content type='html'>I had car trouble on the way to the campus.  It is probably a problem with the coil.  After the car sat immobile for a while, I managed to get it cranked, but as I didn't want to get stranded at Covington at 11 PM, I needed to drive it back home so I can work on it over the weekend.&lt;br /&gt;&lt;br /&gt;For lecture on Tuesday, we will do the Part II of the Georgia Geology Notes and start on Chapter 9 - Geologic Time.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2009584220242349548?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2009584220242349548/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2009584220242349548' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2009584220242349548'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2009584220242349548'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/06/sorry-for-missing-class.html' title='Sorry for Missing Class'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1559562811583571736</id><published>2008-06-23T11:50:00.000-04:00</published><updated>2008-06-24T08:29:09.501-04:00</updated><title type='text'>Exam II Review</title><content type='html'>&lt;strong&gt;Chapter 6&lt;/strong&gt;&lt;br /&gt;&gt;Remember the difference between Physical Weathering and Chemical Weathering. &lt;strong&gt;Hydrolysis&lt;/strong&gt; is the type of Chemical Weathering that &lt;strong&gt;changes feldspar to kaolinite clay&lt;/strong&gt;.&lt;br /&gt;&gt;The exfoliation sheeting that produced the rounded shape of Stone Mt. is a type of Physical Weathering. Root wedging is also a type of Physical Weathering. So is Frost Wedging.&lt;br /&gt;&gt;Remember the definition of Erosion. And that the principle agent of erosion is moving water.&lt;br /&gt;&gt;"Mass Wasting" is a fancy term for landslides, mudslides, etc..&lt;br /&gt;&gt;Physical Weathering does not change the chemistry of the rock or mineral. Physical Weathering produces more surface area by breaking up the rock or mineral and facilitates Chemical Weathering.&lt;br /&gt;&gt;Water can cause Mass Wasting events because it is heavy and it acts as a lubricant for gravity-produced soil and rock movement.&lt;br /&gt;&gt;The &lt;strong&gt;dissolution &lt;/strong&gt;of &lt;strong&gt;calcite in limestone/marble&lt;/strong&gt; is responsible for the formation of most caverns.&lt;br /&gt;&gt;All of the important &lt;strong&gt;Silicate&lt;/strong&gt; &lt;strong&gt;minerals&lt;/strong&gt; are susceptible to &lt;strong&gt;hydrolysis&lt;/strong&gt;, &lt;strong&gt;except quartz&lt;/strong&gt;.&lt;br /&gt;&gt;The &lt;strong&gt;rounded granite boulders&lt;/strong&gt; at Charlie Elliott Nature Center (and elsewhere) are produced by &lt;strong&gt;Spheroidal Weathering&lt;/strong&gt;.&lt;br /&gt;&gt;Remember the definition of "saprolite".&lt;br /&gt;&gt;&lt;strong&gt;Warm, humid climates&lt;/strong&gt; (as we have here) are &lt;strong&gt;most suitable for Chemical Weathering&lt;/strong&gt;.&lt;br /&gt;&gt;Good "O" and "A" layers of soil are responsible for an ecosystem's ability to bounce back from disturbances - "Resiliency".&lt;br /&gt;&gt;Deserts are fragile ecosystems because of poor soil conditions. Lack of moisture inhibits "&lt;strong&gt;nutrient cycling&lt;/strong&gt;" &lt;strong&gt;of organics&lt;/strong&gt;. Dead cactus/other plants crumble and the light organics are blown away in the wind.&lt;br /&gt;&lt;strong&gt;&gt;Peat -&lt;/strong&gt; which is the &lt;strong&gt;first progression towards coal&lt;/strong&gt; - accumulates in marsh and swamp environments, such as in the Mississippi Delta and other coastal locations.&lt;br /&gt;&gt;The &lt;strong&gt;primary mineral&lt;/strong&gt; in &lt;strong&gt;limestone is calcite&lt;/strong&gt;.  Algae removes the calcite from water to use in their internal structures, when the algae die, the calcite particles drop to the ocean bottom.&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Chapter 7&lt;br /&gt;&lt;/strong&gt;&gt;Remember the difference between a breccia and a conglomerate.&lt;br /&gt;&gt;Iron oxide cement in sandstone produces a reddish-brown color. Most light-colored sandstones are Silica-cemented.&lt;br /&gt;&gt;The grain size of sediments is related to the water energy - large grains = high energy.&lt;br /&gt;&gt;Sorting refers to the range of grain sizes in a particular sediment.&lt;br /&gt;&gt;Roundness of sand/pebble grains tells of the "distance of transport", i.e., how far the clast has traveled from its original source.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Chapter 8&lt;/strong&gt;&lt;br /&gt;&gt;Directed pressure produces foliated metamorphic rocks.&lt;br /&gt;&gt;Examples of foliated metamorphic rocks are Slate, Phyllite, Schist, and Gneiss.&lt;br /&gt;&gt;The most common non-foliated metamorphic rocks are Marble and Quartzite.&lt;br /&gt;&gt;Index minerals tell us of the Temperature and Pressure conditions of metamorphism, include garnet, kyanite, chlorite, sillimanite.&lt;br /&gt;&gt;Most of the metamorphic rocks on the Georgia Piedmont are regionally metamorphosed with some local areas of contact metamorphism.&lt;br /&gt;&gt;The Lithonia Gneiss is thought to be a metamorphosed Granite.&lt;br /&gt;&gt;If a rock is composed of small, aligned mica flakes, it is probably metamorphic.  If the mica flakes are larger than 1 inch and randomly-oriented, it is probably an igneous rock.&lt;br /&gt;&lt;br /&gt;Sorry for the delays. More material will start appearing here today (Tuesday).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1559562811583571736?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1559562811583571736/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1559562811583571736' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1559562811583571736'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1559562811583571736'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/06/exam-ii-review.html' title='Exam II Review'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6130002661542231956</id><published>2008-06-03T09:49:00.000-04:00</published><updated>2008-06-03T19:16:01.192-04:00</updated><title type='text'>Link to the Physical Geology Page</title><content type='html'>with the Power Point links.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://facstaff.gpc.edu/~jsummero/PhysicalGeology2007.htm"&gt;http://facstaff.gpc.edu/~jsummero/PhysicalGeology2007.htm&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;I think I got the Power Point links fixed (at about 7 PM).&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6130002661542231956?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6130002661542231956/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6130002661542231956' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6130002661542231956'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6130002661542231956'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/06/temporary-link-to-physical-geology-page.html' title='Link to the Physical Geology Page'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4728933570139481812</id><published>2008-06-03T08:51:00.000-04:00</published><updated>2008-06-03T09:40:53.314-04:00</updated><title type='text'>Oil Rigs and Coral Reefs in Harmony</title><content type='html'>Here is &lt;a href="http://www.townhall.com/columnists/HumbertoFontova/2008/06/02/the_environmental_benefits_of_offshore_drilling"&gt;an article&lt;/a&gt; addressing some of the concerns about offshore drilling in the Gulf of Mexico.&lt;br /&gt;&lt;br /&gt;Offshore oil platforms have operated for decades at the &lt;a href="http://flowergarden.noaa.gov/"&gt;Flower Garden Reef&lt;/a&gt;.  Here is more on &lt;a href="http://sanctuaries.noaa.gov/pgallery/pgflower/pgflower.html"&gt;this reef&lt;/a&gt;, off the Texas/Louisiana coast.  The benefits of rigs to certain organisms are &lt;a href="http://sanctuaries.noaa.gov/pgallery/pgflower/habitats/habitats_8.html"&gt;described here&lt;/a&gt;.  Basically, rigs create new vertical habitats for organisms that must attach to some sort of structure.  Once these attaching organisms are established, other organisms are attracted to the area.  From the following link:&lt;br /&gt;&lt;br /&gt;&lt;em&gt;..."Natural structure and hard bottom are rare in the Gulf of Mexico where the bottom is pretty much a vast featureless plain of mud and sand. Where structure does occur, natural or otherwise, it is like an oasis in a desert. Virtual gardens of sessile (permanently attached) invertebrates like barnacles, corals, sponges, clams, anemones, bryozoans and hydroids quickly attach to every available surface and in every nook and cranny. "...&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;When the well (or wells) "plays out", removing the rig structure would damage the established reef organisms and disrupt the system.  So a program was established to leaf the structures in place (below a certain depth) and use the rig housing as additional structure for reef growth.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.tpwd.state.tx.us/fishboat/fish/didyouknow/reefcreation.phtml"&gt;Rigs-to-Reefs program&lt;/a&gt;.  From this website:&lt;br /&gt;&lt;br /&gt;&lt;em&gt;..."Since 1990, cooperating oil and gas companies have donated more than 64 obsolete petroleum platforms and contributed one half of the savings realized by reefing their rigs to the Artificial Reef Fund. These dedicated funds allow the Program to be relatively self-sufficient and finance research, administration, maintenance, liability coverage and construction of new artificial reefs."...&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;It is possible that the corals and other organisms in this area (SE of Galveston) are simply hardier, due to the natural oil seeps in the bottom of the Gulf.  Whether or not reef organisms, in other areas, would "welcome" oil rigs might be debateable, but the record looks good.  Imagine the disruptive scenario when a well plays out after decades and an emotion-driven eco-Luddite demands total removal of the structure, even that portion well-below the wave base.&lt;br /&gt;&lt;br /&gt;These benefits are brought about by the free-market system and the sensible give-and-take regarding governments and their regulations.  None of this is to suggest that these endeavors are risk-free (that world doesn't exist), but risks can be managed and minimized.  Whether the government-controlled oil companies of China and Venezuela (drilling 50 miles from Key West) concern themselves about the reef organisms remains to be seen.&lt;br /&gt;&lt;br /&gt;Our oil companies do listen to public concerns (maybe too much regarding the carbon dioxide hysteria), but sometimes it takes years to find a solution to address the public concerns.  Government-owned firms may not find Public Relations to be a priority.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4728933570139481812?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4728933570139481812/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4728933570139481812' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4728933570139481812'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4728933570139481812'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/06/oil-rigs-and-coral-reefs-in-harmony.html' title='Oil Rigs and Coral Reefs in Harmony'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4906624407674136107</id><published>2008-05-27T09:42:00.002-04:00</published><updated>2008-05-27T09:51:17.925-04:00</updated><title type='text'>A Few Articles About Present and Future Oil Resources</title><content type='html'>&lt;a href="http://www.anwr.org/case.htm"&gt;The Case for ANWR Development&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.rense.com/general37/petrol.htm"&gt;Canada's Reserves&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;[More will be added.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4906624407674136107?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4906624407674136107/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4906624407674136107' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4906624407674136107'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4906624407674136107'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/05/few-articles-about-present-and-future.html' title='A Few Articles About Present and Future Oil Resources'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-5556931256090273637</id><published>2008-05-27T09:42:00.001-04:00</published><updated>2008-05-27T09:42:18.337-04:00</updated><title type='text'></title><content type='html'>&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-5556931256090273637?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/5556931256090273637/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=5556931256090273637' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5556931256090273637'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/5556931256090273637'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/05/blog-post.html' title=''/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3064996658997100441</id><published>2008-05-24T01:10:00.001-04:00</published><updated>2008-05-24T01:12:57.887-04:00</updated><title type='text'>A Good Yahoo News Article About the "Whys" of Increased Gasoline Prices</title><content type='html'>&lt;a href="http://news.yahoo.com/s/ap/20080523/ap_on_bi_ge/money_in_the_tank"&gt;http://news.yahoo.com/s/ap/20080523/ap_on_bi_ge/money_in_the_tank&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;It is a bit more complex than can be covered in a 15- or 30-second sound byte.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3064996658997100441?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3064996658997100441/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3064996658997100441' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3064996658997100441'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3064996658997100441'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/05/good-yahoo-news-article-about-whys-of.html' title='A Good Yahoo News Article About the &quot;Whys&quot; of Increased Gasoline Prices'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3431577615571300264</id><published>2008-05-06T17:22:00.001-04:00</published><updated>2008-05-06T17:24:02.794-04:00</updated><title type='text'>Last Chance for Final</title><content type='html'>Two of you from my MWF class and one from the MW class missed your final.  The last chance is Wednesday.  I plan to be at the campus at about 11:30 AM to 12 Noon at Room 3250.&lt;br /&gt;&lt;br /&gt;Consequences are either a letter grade lower or an Incomplete.&lt;br /&gt;&lt;br /&gt;Email me.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3431577615571300264?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3431577615571300264/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3431577615571300264' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3431577615571300264'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3431577615571300264'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/05/last-chance-for-final.html' title='Last Chance for Final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-195780217925438035</id><published>2008-05-05T11:56:00.000-04:00</published><updated>2008-05-05T12:00:19.571-04:00</updated><title type='text'>Last Chance for any Extra Credit</title><content type='html'>If any of your are feeling queezy after the final (the MWF class), you still have some time to email me an Annotated Bibliography of Nature-related books, as I explained in class, I will accept them within 24 hours of your finishing your final.  Maybe 36 if I haven't finished all of my grading.  Any points might help.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-195780217925438035?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/195780217925438035/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=195780217925438035' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/195780217925438035'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/195780217925438035'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/05/last-chance-for-any-extra-credit.html' title='Last Chance for any Extra Credit'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-9024888071892176862</id><published>2008-05-05T11:21:00.000-04:00</published><updated>2008-05-05T11:25:25.644-04:00</updated><title type='text'>For Those That Missed the May 5 Final Exam...</title><content type='html'>You need to email me ASAP.  I have one more final tomorrow at 1 PM.  If I have to make an extra trip to Covington, I will not be happy.  Or else you can get a letter grade lower...&lt;br /&gt;&lt;br /&gt;Contact me.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-9024888071892176862?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/9024888071892176862/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=9024888071892176862' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/9024888071892176862'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/9024888071892176862'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/05/for-those-that-missed-may-5-final-exam.html' title='For Those That Missed the May 5 Final Exam...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4213139085955539949</id><published>2008-05-04T21:46:00.000-04:00</published><updated>2008-05-05T17:53:21.843-04:00</updated><title type='text'>A Few Study Tips for the Final</title><content type='html'>Remember, you can have two two-sided sheets of notes for Part II of the final. No notes are allowed for Part I.&lt;br /&gt;&lt;br /&gt;There will be &lt;strong&gt;No Questions on the final - on the following subjects:&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;Katrina, Ethanol, (more will be added as I think about it).&lt;br /&gt;&lt;br /&gt;Some things to study...&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;The Water Cycle; &lt;/li&gt;&lt;li&gt;the Carbon Cycle; &lt;/li&gt;&lt;li&gt;How is the stable N2 converted to the ammonium, nitrate, and nitrite ions needed by plants?;&lt;/li&gt;&lt;li&gt;The difference in Convergent and Divergent Zones and what type of volcanoes are associated with each - explosive composite/stratovolcanoes with Convergent Zones and quieter basaltic eruptions with Divergent Zones and Hot Spots;&lt;/li&gt;&lt;li&gt;Examples of interactions between the Biosphere and the Atmosphere.&lt;/li&gt;&lt;li&gt;The basics of atmospheric composition (most common gas) and different functions of the Troposphere vs. the Stratosphere;&lt;/li&gt;&lt;li&gt;What is used to calculate population growth - birth rates, death rates, immigration, and emigration;&lt;/li&gt;&lt;li&gt;What causes a "J" curve to change to an "S" curve - environmental resistance;&lt;/li&gt;&lt;/ul&gt;&lt;p&gt;More to study (sorry for the delay):&lt;/p&gt;&lt;ul&gt;&lt;li&gt;Aspects of the Scientific Method and &lt;strong&gt;the two ways that the effects of personal bias can be lessened&lt;/strong&gt;.&lt;/li&gt;&lt;li&gt;The difference between &lt;strong&gt;Abiotic&lt;/strong&gt; and &lt;strong&gt;Biotic&lt;/strong&gt; components and examples of each.&lt;/li&gt;&lt;li&gt;The difference between &lt;strong&gt;Species Diversity&lt;/strong&gt; and &lt;strong&gt;Genetic Diversity&lt;/strong&gt;.&lt;/li&gt;&lt;li&gt;The importance of the O and A layers in the soil profile.&lt;/li&gt;&lt;li&gt;What the concept of "&lt;strong&gt;Tragedy of the Commons&lt;/strong&gt;" is and how it might apply to "commonly-owned" resources, such as ocean fisheries.&lt;/li&gt;&lt;li&gt;Definitions and occurrences of "&lt;strong&gt;Orographic Lifting&lt;/strong&gt;" and the "&lt;strong&gt;Rain Shadow Effect&lt;/strong&gt;" and how they apply to the presence of ecosystems in the Western United States, including the &lt;strong&gt;four North American Deserts&lt;/strong&gt;.&lt;/li&gt;&lt;li&gt;The relationship between Mount St. Helens and the subduction zone.&lt;/li&gt;&lt;li&gt;Remember the types of plate tectonics interactions.&lt;/li&gt;&lt;li&gt;Definition of "&lt;strong&gt;Range of Tolerance&lt;/strong&gt;" and how it applied to the story of the "Iceland fisherman".&lt;/li&gt;&lt;li&gt;Defintions of &lt;strong&gt;Keystone Species&lt;/strong&gt;, &lt;strong&gt;Indicator Species&lt;/strong&gt;, &lt;strong&gt;Generalist Species&lt;/strong&gt;, &lt;strong&gt;Specialist Species&lt;/strong&gt;.&lt;/li&gt;&lt;li&gt;Beneficial mutations (traits) and how they must be in place &lt;strong&gt;before environmental changes take place.&lt;/strong&gt;&lt;/li&gt;&lt;li&gt;The characteristics of the &lt;strong&gt;Hadley Cells&lt;/strong&gt; and the &lt;strong&gt;Rossby Regime&lt;/strong&gt;.&lt;/li&gt;&lt;li&gt;Remember that in desert mountain environments, the morning sun is cooler than the afternoon sun, resulting in less evaporation of moisture on the east sides of mountain ranges.&lt;/li&gt;&lt;li&gt;High Pressure Systems - clockwise rotation, falling air.&lt;/li&gt;&lt;li&gt;&lt;strong&gt;Low Pressure Systems&lt;/strong&gt; - &lt;strong&gt;counter-clockwise rotation, rising air&lt;/strong&gt; - most beneficial for the growth of clouds and storms.&lt;/li&gt;&lt;li&gt;&lt;strong&gt;Resiliency&lt;/strong&gt; refers to the ability of an ecosystem to "bounce back" from disturbances.&lt;/li&gt;&lt;li&gt;Which biome/ecosystem in which we live - &lt;strong&gt;Temperate Deciduous&lt;/strong&gt;. Ecosystems are defined by and Abiotic term, then by Biotic term. Usually climate is first, major vegetation is the second.&lt;/li&gt;&lt;li&gt;An Age-Structure Diagram for a constantly-growing population is &lt;strong&gt;shaped like a pyramid&lt;/strong&gt;.&lt;/li&gt;&lt;li&gt;What components of a properly constructed water well are designed to keep surface pollutants out of the aquifer?&lt;/li&gt;&lt;li&gt;Definitions of &lt;strong&gt;Population, Community, Niche, Habitat, Commensalism, Mutualism/Symbiosis &lt;/strong&gt;and examples of Commensalism and Mutualism.&lt;/li&gt;&lt;/ul&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;Remember for Part II, you can have 2 two-sided sheets of notes, as well as the graded Exam IV that will be handed back to you.&lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4213139085955539949?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4213139085955539949/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4213139085955539949' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4213139085955539949'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4213139085955539949'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/04/few-study-tips-for-final.html' title='A Few Study Tips for the Final'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3381450562316547232</id><published>2008-04-30T08:21:00.000-04:00</published><updated>2008-04-30T08:23:52.029-04:00</updated><title type='text'>Notes for the Final...</title><content type='html'>will be appearing sometime today.  I am still getting over being sick on Sunday/Monday.&lt;br /&gt;&lt;br /&gt;As for my MW 12:30 PM class,... Dea K., will you please email me about your needing to take the final early?&lt;br /&gt;&lt;br /&gt;Check back later for study tips.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3381450562316547232?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3381450562316547232/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3381450562316547232' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3381450562316547232'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3381450562316547232'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/04/notes-for-final.html' title='Notes for the Final...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6639739620853943468</id><published>2008-04-28T10:01:00.000-04:00</published><updated>2008-04-28T10:05:53.305-04:00</updated><title type='text'>A Note to Students in Both Classes</title><content type='html'>I apologize for not being there to hand back your Exam IV papers and other materials.  I have been sick since yesterday afternoon.  Please email me at my hotmail account tomorrow and I can give you the exam IV grade.  &lt;a href="mailto:jsummerour@hotmail.com"&gt;jsummerour@hotmail.com&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;I will be posting info here for final exam review.  Keep checking back throughout the week.&lt;br /&gt;&lt;br /&gt;Final exam schedule (may be slightly different from what I told you in class).&lt;br /&gt;&lt;br /&gt;MWF 11 AM class - May 5, 10:30 AM, Room 3250&lt;br /&gt;&lt;br /&gt;MW 12:30 PM class 0 May 6, 1 PM, Room 3250&lt;br /&gt;&lt;br /&gt;I apologize for the inconvenience.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6639739620853943468?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6639739620853943468/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6639739620853943468' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6639739620853943468'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6639739620853943468'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/04/note-to-students-in-both-classes.html' title='A Note to Students in Both Classes'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1113268980021113643</id><published>2008-04-24T09:57:00.000-04:00</published><updated>2008-04-24T09:59:24.090-04:00</updated><title type='text'>Note to Students in my MWF morning class...</title><content type='html'>There are 50 Assessment questions, not 100.&lt;br /&gt;&lt;br /&gt;It is vitally important that you be in class Friday and Monday.&lt;br /&gt;&lt;br /&gt;Some review notes may be posted here and perhaps on my website if I can get them to upload on Friday.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1113268980021113643?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1113268980021113643/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1113268980021113643' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1113268980021113643'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1113268980021113643'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/04/note-to-students-in-my-mwf-morning.html' title='Note to Students in my MWF morning class...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2267043708930870928</id><published>2008-04-20T20:36:00.000-04:00</published><updated>2008-04-21T12:18:00.035-04:00</updated><title type='text'>Links for Env. Science Exam IV</title><content type='html'>More will be added, if deemed necessary.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.cbu.edu/~seisen/Demography/sld016.htm"&gt;Age Structure Diagram&lt;/a&gt; Question 11&lt;br /&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Directional_drilling"&gt;Directional Drilling&lt;/a&gt; Question 12&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.foxnews.com/story/0,2933,349728,00.html"&gt;Fox News Story on Bakken Formation&lt;/a&gt; Question 13&lt;br /&gt;&lt;br /&gt;&lt;a href="http://en.wikipedia.org/wiki/Bakken_Formation"&gt;More info on the Bakken Formation&lt;/a&gt; Question 13&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.anwr.org/case.htm"&gt;Arguments in favor of ANWR development&lt;/a&gt; Question 14&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.chem.tamu.edu/class/majors/msdsfiles/msdsammonia.htm"&gt;MSDS Form for Ammonia&lt;/a&gt; Question 17&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.epa.gov/epahome/r2k.htm"&gt;Right to Know Laws&lt;/a&gt; Question 18&lt;br /&gt;&lt;br /&gt;[Update: If you don't have time to do a full term paper to help your average, you can do an Annotated Bibliography (perhaps 5 pages) of nature-related books, with a short descriptive entry for each one, telling what the book is about.  I may decide to let you add another page listing local nature-related organizations, e.g., the Georgia Native Plant Society.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2267043708930870928?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2267043708930870928/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2267043708930870928' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2267043708930870928'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2267043708930870928'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/04/links-for-env-science-exam-iv.html' title='Links for Env. Science Exam IV'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-1483022738991611334</id><published>2008-04-02T06:35:00.000-04:00</published><updated>2008-04-02T07:53:08.851-04:00</updated><title type='text'>A Few Considerations on Current Events</title><content type='html'>By way of &lt;a href="http://www.newsbusters.org/"&gt;NewsBusters&lt;/a&gt; is this &lt;a href="http://proteinwisdom.com/?p=11645"&gt;Protein Wisdom post&lt;/a&gt; on the April Fool's Day Congressional hearings to "gin-up" some scapegoats for this election season.&lt;br /&gt;&lt;br /&gt;Embedded with the Protein Wisdom post is &lt;a href="http://www.businessandmedia.org/specialreports/2008/MediaMyth/Crude_Coverage/CrudeCompany.asp"&gt;this link&lt;/a&gt; to a Business and Media Institute article reminding us of OPEC's influence on the oil markets. Also within the BMI article is this reminder of the realities of the "oil biz".&lt;br /&gt;&lt;br /&gt;Quoting from the article:&lt;br /&gt;&lt;br /&gt;&lt;em&gt;"...ExxonMobil &lt;/em&gt;&lt;a style="COLOR: blue; TEXT-DECORATION: underline; text-underline: single" href="http://www.businesswire.com/portal/site/exxonmobil/index.jsp?ndmViewId=news_view&amp;amp;ndmConfigId=1001106&amp;amp;newsId=20080201005420&amp;amp;newsLang=en&amp;amp;vnsId=-2147483648"&gt;&lt;em&gt;reported $404.6 billion in revenue&lt;/em&gt;&lt;/a&gt;&lt;em&gt; in 2007. It reported $40.6 billion in profits." &lt;/em&gt;&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;And ExxonMobil paid $105 billion in taxes in 2007. &lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Their profit margin is about 10%, industry-wide the profit margin ranges from 7 - 10%, well within the norm of American businesses on Wall Street. This has not changed in the recent years.&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;If Talking Heads and Politicians told you the first two facts, in a court-of-law, without telling you the third one, that would amount to perjury.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-1483022738991611334?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/1483022738991611334/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=1483022738991611334' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1483022738991611334'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/1483022738991611334'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/04/by-way-of-newsbusters-is-this-protein.html' title='A Few Considerations on Current Events'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-8263255857755212312</id><published>2008-03-12T08:41:00.000-04:00</published><updated>2008-03-18T23:18:48.660-04:00</updated><title type='text'>The Problems with Corn-Based Ethanol</title><content type='html'>Here are a few opinion columns and articles... From sources Conservative, Libertarian, and Liberal.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.townhall.com/columnists/WalterEWilliams/2008/03/12/big_corn_and_ethanol_hoax"&gt;Dr. Walter Williams&lt;/a&gt;, &lt;a href="http://sayanythingblog.com/readers/entry/another_ethanol_negative_water_consumption/"&gt;Say Anything Blog&lt;/a&gt;, &lt;a href="http://www.cato.org/pub_display.php?pub_id=7308"&gt;Cato Institute&lt;/a&gt;, &lt;a href="http://www.tcsdaily.com/article.aspx?id=071206E"&gt;Tech Central Station&lt;/a&gt;, &lt;a href="http://hoosier.sierraclub.org/chapter/n0009.html"&gt;Indiana Chapter Sierra Club&lt;/a&gt;, &lt;a href="http://www.slate.com/id/2122961/"&gt;Slate.com&lt;/a&gt;, &lt;a href="http://www.reason.com/blog/show/116529.html"&gt;Reason Hit &amp;amp; Run&lt;/a&gt;, &lt;a href="http://www.usatoday.com/tech/news/2006-07-10-ethanol-study_x.htm"&gt;USA Today&lt;/a&gt;, &lt;a href="http://crufty.blogspot.com/2006/05/problem-with-ethanol.html"&gt;Crosspatch Chronicle Blog&lt;/a&gt;.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-8263255857755212312?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/8263255857755212312/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=8263255857755212312' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8263255857755212312'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8263255857755212312'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/03/problems-with-corn-based-ethanol.html' title='The Problems with Corn-Based Ethanol'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7348868889754945092</id><published>2008-01-14T09:17:00.000-05:00</published><updated>2008-01-14T08:01:18.098-05:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Environmental News'/><title type='text'>Monday Round-up #1</title><content type='html'>Pertinent environmental news...&lt;br /&gt;&lt;br /&gt;**&lt;a href="http://environment.independent.co.uk/climate_change/article3333872.ece"&gt;World Bank actions result in loss of Brazilian rain forest&lt;/a&gt;. World Bank pledges to help save rain forests, then makes loans to help expand Brazilian cattle farms, soy farms for cattle feed, and sugar cane production (for biofuels).&lt;br /&gt;&lt;br /&gt;**Sunday AJC Letter-to-the-Editor writer: "World population must go in reverse."&lt;br /&gt;&lt;br /&gt;To "solve" overpopulation problem&lt;em&gt;..."All the world's people must collectively reduce world human population to probably 5 percent to 10 percent of its current level, while raising the quality of living of all. This is a social decision. Technology will not save us."...&lt;/em&gt;&lt;br /&gt;&lt;em&gt;&lt;/em&gt;&lt;br /&gt;**&lt;a href="http://newsbusters.org/blogs/noel-sheppard/2008/01/13/rare-snows-cold-saudi-arabia-ignored-us-media"&gt;Saudi Arabia has its coldest winter in 20 years&lt;/a&gt;. Snow and sub-zero temperatures in Saudi Arabia, light snow in Baghdad.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7348868889754945092?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7348868889754945092/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7348868889754945092' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7348868889754945092'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7348868889754945092'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2008/01/monday-round-up-1.html' title='Monday Round-up #1'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-4464118319296492512</id><published>2007-07-22T17:07:00.000-04:00</published><updated>2007-07-22T17:11:43.305-04:00</updated><title type='text'>A Few More Exam III Reminders</title><content type='html'>In the nutrient cycles, remember the characteristics of Nitrogen, Phosphorous, why excess Sulfur gases are harmful.&lt;br /&gt;&lt;br /&gt;What part of the Water Cycle is represented by the formation of clouds and how does it happen?&lt;br /&gt;&lt;br /&gt;Remember what diurnal temperature variation is and how the Greenhouse Effect affects it.&lt;br /&gt;&lt;br /&gt;More to come...&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-4464118319296492512?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/4464118319296492512/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=4464118319296492512' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4464118319296492512'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/4464118319296492512'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/07/few-more-exam-iii-reminders.html' title='A Few More Exam III Reminders'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-3370589675128787522</id><published>2007-07-22T13:23:00.000-04:00</published><updated>2007-07-22T13:38:46.319-04:00</updated><title type='text'>Hurricane Katrina DVD Questions and Answers</title><content type='html'>1.  The low-pressure system that became Katrina began where?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;Off the west coast of Africa&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;2.  These weather systems are characterized by what direction of rotation?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;Counter-clockwise&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;3.  Which 2004 hurricane proved a close call for New Orleans?&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;&lt;em&gt;Ivan&lt;/em&gt;&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;4.  During the hurrican-chasing airplane flights, what are the functions of a "drop sonde"?&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;&lt;em&gt;Collecting data on wind speeds &amp; directions, temperatures, etc.&lt;/em&gt;&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;5.  What are the two things that help "guide" a hurricane?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;High-Pressure and Low-Pressure zones, sometimes strong weather fronts.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;6.  To what is attributed 90% of hurricane deaths?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;Drowning in storm surges.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;7.  The oldest parts of New Orleans are built upon natural levees which are located where?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;The French Quarter, next to the river.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;8.  What allowed the growth of the city away from the natural levees?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;The development of a pumping system that allowed the drainage of wetlands.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;9.  What are the two types of levees in the New Orleans area?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;Earthen levees and Concrete/Steel floodwalls.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;10.  Considering the direction of rotation of the hurricane, where is the strongest part?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;The Eastern or Northeastern part is the strongest.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;11.  What human activity resulted in the degradation of the Mississippi River delta wetlands?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;Levee enhancements and channel control prevented the normal replenishment of silt by yearly flooding.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;12.  The Lower Ninth Ward was flooded after a 15-foot high storm surge on the Intercoastal Waterway caused the breaching of the levee along which waterway"&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;The Industrial Canal.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;13.  In the other DVD, a 21 foot-high storm surge along the Mississippi Coast was reported during Hurricane Camille (1969).  How high was the Hurricane Katrina storm surge in the same area?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;28 feet.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;14.  The flooding of most of downtown New Orleans was caused by breachments of which two canals?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;London Ave. and 17th Street canals.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;15.  Regarding past cycles of hurricane activity, the 1940s through 1960s (approximately) cycle coincided with a minor period of &lt;strong&gt;climatic cooling.  &lt;/strong&gt;Was this period an active cycle or inactive cycle?&lt;br /&gt;&lt;br /&gt;&lt;em&gt;&lt;strong&gt;Active.&lt;/strong&gt;&lt;/em&gt;&lt;br /&gt;&lt;br /&gt;Sorry for the delay.  Have been busy with my second job.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-3370589675128787522?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/3370589675128787522/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=3370589675128787522' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3370589675128787522'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/3370589675128787522'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/07/hurricane-katrina-dvd-questions-and.html' title='Hurricane Katrina DVD Questions and Answers'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-8855176084135766790</id><published>2007-07-19T00:39:00.000-04:00</published><updated>2007-07-19T00:44:55.757-04:00</updated><title type='text'>A Few Reminders for Exam III</title><content type='html'>Of the natural sources of carbon dioxide, the largest is probably Ocean releases, considering that 71% of the Earth's surface is covered by oceans.&lt;br /&gt;&lt;br /&gt;When looking at clouds, clouds that look like "heaps" are of the Cumulus family.&lt;br /&gt;&lt;br /&gt;The most important function of the Gulf Stream is to move heat from the tropics to the northern latitudes.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;[Note - it is OK to have a single-sided sheet of notes for Exam III].&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;More may follow in the next few days.  I covered most everything else in class review.&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-8855176084135766790?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/8855176084135766790/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=8855176084135766790' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8855176084135766790'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8855176084135766790'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/07/few-reminders-for-exam-iii.html' title='A Few Reminders for Exam III'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7839950005206590885</id><published>2007-07-17T09:15:00.000-04:00</published><updated>2007-07-17T05:55:41.239-04:00</updated><title type='text'>Instructions for Environmental Science Exam IV - Summer 2007</title><content type='html'>Vermiculite impurities from the EPA website links are &lt;a href="http://www.epa.gov/asbestos/pubs/verm.html"&gt;here&lt;/a&gt; and &lt;a href="http://www.epa.gov/asbestos/pubs/oppt.pdf"&gt;here&lt;/a&gt;. [If you need to, do a word search for vermiculite and asbestos to see what is found.]&lt;br /&gt;&lt;br /&gt;Another useful website is &lt;a href="http://www.davidcole.net/asbestos/vermiculite.html"&gt;here&lt;/a&gt;. &lt;strong&gt;[Certain computers may have a problem with this particular website. Will try to determine what the problem is, the message is something about a Flash Media add-on problem.]&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;This information, as was stated, may be of use in your future.&lt;br /&gt;&lt;br /&gt;Allow yourself time to find the information, it is there, it just takes some diligence.&lt;br /&gt;&lt;br /&gt;For Question 13, check out the Conservation link at the El Paso Water Utilities website.&lt;br /&gt;&lt;br /&gt;Notes on Question 16:&lt;br /&gt;&lt;br /&gt;Since we did not cover Chapter 8, you do not have to do Question 16, but if you want to, there might be some extra points awarded.&lt;br /&gt;&lt;br /&gt;[Update: Chapter 8 Power Point Notes are accessible on the Environmental Science webpage. They may not correspond to the current textbook, but they will work for this test, if you choose to do Question 16.]&lt;br /&gt;&lt;br /&gt;If you encounter a classmate that wasn't in class for the announcements, let them know about where to find the info. And remind them of the deadlines.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;6/12/07 10:20 AM - Keep checking back here in case there are more updates.&lt;/span&gt;&lt;/strong&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7839950005206590885?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7839950005206590885/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7839950005206590885' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7839950005206590885'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7839950005206590885'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/04/spring-2007-exam-iv.html' title='Instructions for Environmental Science Exam IV - Summer 2007'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-7608992386046693981</id><published>2007-06-27T14:39:00.000-04:00</published><updated>2007-06-27T16:20:09.911-04:00</updated><title type='text'>Attention - MW Night Class...</title><content type='html'>In lieu of class on Mondy, July 2, you have been given assignments to complete, each of which will count as an in-class quiz.&lt;br /&gt;&lt;br /&gt;All three of the cited articles are included on your CD.&lt;br /&gt;&lt;br /&gt;If for some reason you do not have your CD, here are the articles. You will have to ask a classmate for copies of the Homework questions on the CD (the first two) and then the third one, which was handed out in class.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.geocraft.com/WVFossils/greenhouse_data.html"&gt;Water Vapor Rules the Greenhouse&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;&lt;a href="http://www.john-daly.com/history.htm"&gt;Global Warming: How it all Began&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;From the &lt;a href="http://www.friendsofscience.org/index.php?ide=7"&gt;Friends of Science website&lt;/a&gt;:&lt;br /&gt;&lt;br /&gt;Spencer, R.W., and J.R. Christy, 2003: &lt;a href="http://www.friendsofscience.org/documents/Christy-Spencer%20Glob%20Temp%201978-2003.pdf" target="_blank"&gt;Global Temperature Report&lt;/a&gt;, 1978-2003.&lt;br /&gt;&lt;br /&gt;Also, during the break, print out the questions sheet for the Solar Energy DVD.&lt;br /&gt;&lt;br /&gt;Check back for more info.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-7608992386046693981?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/7608992386046693981/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=7608992386046693981' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7608992386046693981'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/7608992386046693981'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/06/attention-mw-night-class.html' title='Attention - MW Night Class...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-6606972216368420431</id><published>2007-06-03T23:50:00.000-04:00</published><updated>2007-06-04T00:27:20.028-04:00</updated><title type='text'>Exam II Tips - For the Morning Class</title><content type='html'>You need to remember the relationships shown on Geology Composite Power Point slide #2, the Orographic Effect and how it works on the windward and leeward sides of the mountains. Remember Orographic Lifting and the Rain Shadow Effect.&lt;br /&gt;&lt;br /&gt;Also remember how it affects local weather and climate. [A tip - Weather represents the short-term atmospheric conditions and events. Climate represents 30-year or longer averages.]&lt;br /&gt;&lt;br /&gt;Remember why Plate Tectonics is called a "Unifying Theory".&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Other things to remember about Plate Tectonics:&lt;br /&gt;&lt;/strong&gt;&lt;br /&gt;The most important early proponent, who did not live to see his hypothesis become theory in the mid-1970s.&lt;br /&gt;&lt;br /&gt;Remember some of the evidence that the continents were once joined.&lt;br /&gt;&lt;br /&gt;Remember what wartime technologies we employed to map the ocean bottoms after WWII.&lt;br /&gt;&lt;br /&gt;Remember what "Isostacy" means.&lt;br /&gt;&lt;br /&gt;Remember the types of plate interactions and their synonyms.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Divergent zone/Rift zone&lt;/strong&gt; - where plates are separating slowly. If Rift Zones, volcanic rocks are usually &lt;strong&gt;Basaltic (or Mafic)&lt;/strong&gt; because the crust is thin, allowing molten rock to rise directly from the &lt;strong&gt;mantle&lt;/strong&gt;.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Convergent zone/Subduction zone&lt;/strong&gt; - where one plate is sliding beneath another. The sinking plate melts, triggering volcanism inland from the subduction zone. Volcanic rocks are &lt;strong&gt;andesitic (or intermediate)&lt;/strong&gt; and &lt;strong&gt;are more explosive&lt;/strong&gt; than the Basaltic/Mafic rocks &lt;strong&gt;because of the increased quartz content&lt;/strong&gt;. These types of volcanoes are called &lt;strong&gt;Composite/Stratovolcanoes&lt;/strong&gt; and examples include Mount St. Helens, Mt. Pinatubo, El Chichon, Galeras Volcano (from the DVD). The Cascade Mts. in the NW United States are an example of a Continental Arc System. Where one oceanic plate slides beneath another, it forms an Island Arc System, example Japan, Aleutians.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Transform fault zones&lt;/strong&gt; - are where one plate slides past another. Volcanoes are rare or absent from this particular type of plate interaction. The San Andreas Fault Zone in California is an example of this.&lt;br /&gt;&lt;br /&gt;Know the composition of Oceanic Crust - Gabbro (or Mafic) and Continental Crust - Granite (or Felsic).&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Weathering&lt;/strong&gt; breaks down rocks by natural processes and &lt;strong&gt;erosion&lt;/strong&gt; carries the particles to the ocean. &lt;strong&gt;Chemical weathering&lt;/strong&gt; dissolves the minerals. &lt;strong&gt;Physical weathering&lt;/strong&gt; breaks down minerals through frost action and other processes.&lt;br /&gt;&lt;br /&gt;In a stream, the size of the sediment particles is related to the &lt;strong&gt;stream energy&lt;/strong&gt;, which is an abiotic component. The faster moving waters of mountain streams washes out the smaller particles, leaving the larger ones behind.&lt;br /&gt;&lt;br /&gt;On the continental shelves, sediment particles are distributed based on grain size, with the largest grains along the shoreline in the high energy surf zone. The grain sizes decrease away from the shoreline, as the waters become quieter.&lt;br /&gt;&lt;br /&gt;Most sedimentary rocks were deposited in shallow marine conditions, either on continental shelves, similar to today or in shallow, inland seas that covered much of the North American continent during the Paleozoic Era.  These types of environments, warm, shallow marine ecosystems generally have the greatest species diversity.&lt;br /&gt;&lt;br /&gt;Remember the differences and locations of rocky shore habitats and sandy shore habitats.  Remember which one is &lt;strong&gt;submergent&lt;/strong&gt; and which one is &lt;strong&gt;emergent.&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;[More will be added.]&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-6606972216368420431?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/6606972216368420431/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=6606972216368420431' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6606972216368420431'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/6606972216368420431'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/06/exam-ii-tips-for-morning-class.html' title='Exam II Tips - For the Morning Class'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2060237627543275730</id><published>2007-05-23T06:53:00.000-04:00</published><updated>2007-05-23T06:56:10.084-04:00</updated><title type='text'>A Noteworthy Article on Corn-Based Ethanol</title><content type='html'>John Stossel has &lt;a href="http://www.townhall.com/columnists/column.aspx?UrlTitle=the_many_myths_of_ethanol&amp;ns=JohnStossel&amp;amp;dt=05/23/2007&amp;page=full&amp;amp;comments=true"&gt;this article&lt;/a&gt; on the problems associated with corn-based ethanol.&lt;br /&gt;&lt;br /&gt;There may be a homework assignment on this article and other current events articles in the near future.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2060237627543275730?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2060237627543275730/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2060237627543275730' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2060237627543275730'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2060237627543275730'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/05/noteworthy-article-on-corn-based.html' title='A Noteworthy Article on Corn-Based Ethanol'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-108793362753357642</id><published>2007-05-02T09:58:00.002-04:00</published><updated>2007-05-02T11:19:25.769-04:00</updated><title type='text'>ENVIRONMENTAL SCIENCE STUDENTS...</title><content type='html'>Keep watching this space for Final Exam Updates.&lt;br /&gt;&lt;br /&gt;They are in progress.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;MWF Class - Final Exam - Tuesday May 8 - 8 AM&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;TR Class - Final Exam - Friday May 4 - 1 PM&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Exam IV materials that might be on Final include:&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;Proper orientations for Solar features and what might prevent your adding solar to an existing home (this is in Chapter 13 Power Point).&lt;br /&gt;&lt;br /&gt;General definition of Due Diligence.&lt;br /&gt;&lt;br /&gt;Vermiculite insulation.&lt;br /&gt;&lt;br /&gt;Know the difference between the following previous periods of natural global warming - The Holocene Maximum, the Roman Warm Period, and the Medieval Warm Period. Go on the internet if you need to get approximate dates.&lt;br /&gt;&lt;br /&gt;Purpose of MSDS forms and where they should be stored at a work site.&lt;br /&gt;&lt;br /&gt;Xeriscaping - what it is and its purpose.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Other stuff, from before Exam IV.&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;Know the following terms and what they mean:&lt;br /&gt;&lt;br /&gt;Generalist Species, Specialist Species, Indicator Species, Keystone Species.&lt;br /&gt;&lt;br /&gt;Range of Tolerance, Secondary Succession vs. Primary Succession.&lt;br /&gt;&lt;br /&gt;Why reefs are important marine ecosystems and what threatens them.&lt;br /&gt;&lt;br /&gt;Know four Georgia Geologic Provinces &amp; basic characteristics. Where are the granites? Where is the marble produced? Where is the kaolin produced? All three of the products produce hundreds of jobs in Georgia, if not thousands.&lt;br /&gt;&lt;br /&gt;Most important water well construction features that protect from surface pollutants - concrete surface pad and grout.&lt;br /&gt;&lt;br /&gt;Orographic Effect, Rain Shadow Effect, 4 North American Temperate Deserts and why they exist.&lt;br /&gt;&lt;br /&gt;The basics of the Greenhouse Effect (remember links from Exam IV) and how this affects Diurnal Temperature Variations.&lt;br /&gt;&lt;br /&gt;Know the meaning of &lt;strong&gt;Synergy&lt;/strong&gt; and &lt;strong&gt;Correlation.  &lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Synergy&lt;/strong&gt; is when two environmental inputs combine to produce an effect greater than the effects of the individual inputs.  Example: Trees can become stressed by adverse conditions, such as a excessive rain.  The stress of the excessive rain makes the trees more susceptible to damage by fungus, so the combined effects of rain and fungus is &lt;strong&gt;synergy.&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Correlation&lt;/strong&gt; is when two things happen "about the same time", but they may or may not be related.  Temperature and Carbon Dioxide graphs show a correlation between the two values, but it doesn't tell us to which extent they are related nor which one "leads".&lt;br /&gt;&lt;br /&gt;Be aware of the basics of the &lt;strong&gt;Wise Use Movement,&lt;/strong&gt; as presented in the Power Point notes.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-108793362753357642?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/108793362753357642/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=108793362753357642' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/108793362753357642'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/108793362753357642'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/05/environmental-science-students.html' title='ENVIRONMENTAL SCIENCE STUDENTS...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-8581087333344177520</id><published>2007-05-02T09:58:00.001-04:00</published><updated>2007-05-03T00:03:23.753-04:00</updated><title type='text'>PHYSICAL GEOLOGY STUDENTS...</title><content type='html'>Keep watching this space for Final exam study tips.&lt;br /&gt;&lt;br /&gt;Final exam - May 8 - 3:30 PM&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Materials from Exam IV (and other stuff covered after Exam III - Chapter 15 &amp; 16) that might be on the Final Exam:&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;Where does the bulk of the erosion happen &lt;strong&gt;in a meandering stream?&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Basics of mass-wasting&lt;/strong&gt; - the role of gravity and water.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;From Mass Wasting Chapter 15 - &lt;/strong&gt;Remember definitions of Oversteepening, Slumps, Triggering Events.&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;From Running Water Chapter 16 -&lt;/strong&gt; Remember definitions of Competence, Capacity, Bed Load, Suspended Load, Base Level, Stream Gradient, Drainage Basins (or Watersheds) - and in what drainage basin are we located (at the college)?&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;From Ground Water Chapter 17  - &lt;/strong&gt;Remember definitions of Aquifer, Confining Layer, Saturated Zone, Cone of Depression, Annular Space, Surface Pad, Grout, Recharge.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;&lt;span style="font-size:130%;"&gt;Stuff from other chapters - &lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Remember contributions of each&lt;/strong&gt; - Nicolas Steno, William Smith, James Hutton.&lt;br /&gt;&lt;strong&gt;&lt;/strong&gt;&lt;br /&gt;&lt;strong&gt;Plate Tectonics - &lt;/strong&gt;Average compositions of oceanic crust and continental crust.  Remember the three types of plate interactions and examples of each.  What types of plate interactions are related to which types of volcanoes?&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Rock Cycle - &lt;/strong&gt;Basics, Differences between Physical Weathering and Chemical Weathering and Erosion.  What conditions are most conducive to Chemical Weathering, what conditions are most conducive to Physical Weathering - and where does most weathering take place?  Soil type examples - this area - Pedalfers; El Paso - Pedocals; Tropical Rain Forest - Laterites.  Know basics of soils - importance of "O" and "A" layers and their importance to plants.  Know the difference between Internal Processes and External Processes.  What is Carbonic Acid and how does it form in nature?&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Minerals - Basics of Bowen Reaction Series and what class of minerals does it address&lt;/strong&gt;?  What are the 3 emphasized characteristics of minerals?  What do you first notice about a mineral and why might that feature be an unreliable way to identify the mineral?  How do we classify minerals?&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Igneous Rocks - &lt;/strong&gt;Difference between Mafic and Felsic minerals and rocks.  Know the difference between aphanitic and phaneritic and how they form.  How do porphyritic rocks form?  Why are there vesicles in some volcanic rocks?   Remember the intrusive/extrusive associations - Gabbro/Basalt; Diorite/Andesite; Granite/Rhyolite.  &lt;strong&gt;Remember the difference between a dike and a sill.&lt;/strong&gt;  Remember the rock types associated with shield volcanoes and composite volcanoes, as well as the definitions of these rocks.&lt;br /&gt;&lt;br /&gt;More information will be added.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-8581087333344177520?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/8581087333344177520/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=8581087333344177520' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8581087333344177520'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/8581087333344177520'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/05/physical-geology-students.html' title='PHYSICAL GEOLOGY STUDENTS...'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-2671400547236945270</id><published>2007-04-23T09:10:00.000-04:00</published><updated>2007-04-25T08:35:15.683-04:00</updated><title type='text'>Instructions for Physical Geology Exam IV</title><content type='html'>&lt;strong&gt;This exam is due Tuesday, May 1. I will take it after that, but arrangements will have to be made to find me and points will be counted off.&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;Sorry for the late date, but that is the way things work out. &lt;strong&gt;Class Attendance for Thursday April 26 is optional, but suggested for the purpose of review.&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;Check the websites linked in the box. If need be, go back and check the &lt;a href="http://www.gpc.edu/~jsummero/GaGeolNotesPreferred.ppt"&gt;Georgia Geology&lt;/a&gt; Power Point links from lecture, earlier in the semester.&lt;br /&gt;&lt;br /&gt;For Question 13, you may have to do some more &lt;span class="blsp-spelling-error" id="SPELLING_ERROR_0"&gt;internet&lt;/span&gt; research beyond this &lt;span class="blsp-spelling-error" id="SPELLING_ERROR_1"&gt;Gwinnett&lt;/span&gt; County Department of Public Utilities &lt;a href="http://www.co.gwinnett.ga.us/departments/publicutilities/pdf/waterwords_2005.pdf"&gt;&lt;span class="blsp-spelling-error" id="SPELLING_ERROR_2"&gt;webpage&lt;/span&gt;&lt;/a&gt;. Here is &lt;a href="http://www.gwf.org/gawater/RiverBasinsFinal.pdf"&gt;a map&lt;/a&gt; of Georgia's 14 River Basins.&lt;br /&gt;&lt;br /&gt;There is a "typo" in the second question within #13 - It should read:&lt;br /&gt;&lt;br /&gt;"Into &lt;strong&gt;which&lt;/strong&gt; river basin does most of &lt;span class="blsp-spelling-error" id="SPELLING_ERROR_3"&gt;Gwinnett&lt;/span&gt; County's sewers drain?"&lt;br /&gt;&lt;br /&gt;Here is some more useful info for Question 13:&lt;br /&gt;&lt;br /&gt;'&lt;span class="blsp-spelling-error" id="SPELLING_ERROR_4"&gt;Interbasin&lt;/span&gt; transfer' means the withdrawal, diversion, or pumping of surface waters from a point within any basin of origin and the discharge of all or any part of that water into a different receiving basin by means of pipes, conduits, ditches, or canals.&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;If I &lt;span class="blsp-spelling-corrected" id="SPELLING_ERROR_5"&gt;inadvertently used "intrabasin transfer" in the Power Point or elsewhere, that means water transfers within the same basin.&lt;/span&gt;&lt;/strong&gt;&lt;br /&gt;&lt;br /&gt;Questions 14 through 18 are largely from Chapter 16, on Running Water - go the &lt;a href="http://www.gpc.edu/~jsummero/PhyGeolCh16new.ppt"&gt;Power Point&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;Question19 through 23 are largely from Chapter 17, on Ground Water - go to the &lt;a href="http://www.gpc.edu/~jsummero/PhyGeolCh17new.ppt"&gt;Power Point&lt;/a&gt;.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-2671400547236945270?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/2671400547236945270/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=2671400547236945270' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2671400547236945270'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/2671400547236945270'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2007/04/instructions-for-physical-geology-exam.html' title='Instructions for Physical Geology Exam IV'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-266113270994754624</id><published>2006-11-15T14:30:00.000-05:00</published><updated>2007-04-23T10:12:11.348-04:00</updated><title type='text'>Watch This Space for Exam IV Information - 2006</title><content type='html'>Question 1 (short essay) concerns the Burgess Shale, check Chapter 12 Power Point, Dr. Pam Gore's &lt;a href="http://www.gpc.edu/~pgore/geology/geo102/burgess/burgess.htm"&gt;Burgess Shale&lt;/a&gt; webpage, &amp; Dr. Gore's &lt;a href="http://gpc.edu/~pgore/geology/geo102/cambrian.htm"&gt;Cambrian Period&lt;/a&gt; webpage for information.&lt;br /&gt;&lt;br /&gt;Questions 2 - 10 are fill-in-the-blank, using the A-N answers. Information is from Chapter 10 - 12 Power Point and other sources (as needed), including some of Dr. Gore's webpages. You will not use all of the answers.&lt;br /&gt;&lt;br /&gt;For Questions 11 - 26, check the Chapter 10 - 13 Power Point notes and Dr. Gore's webpages in the green box on your instructor's &lt;a href="http://www.gpc.edu/~jsummero/HistGeol2006.htm"&gt;Historical Geology webpage&lt;/a&gt;.&lt;br /&gt;&lt;br /&gt;Questions 27 &amp;amp; 28 are from the &lt;a href="http://www.geocraft.com/WVFossils/TableOfCont.html"&gt;Plant Fossils of West Virginia&lt;/a&gt; website. This website is pertinent because some of these same plant fossils occur in Dade County, GA.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-266113270994754624?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/266113270994754624/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=266113270994754624' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/266113270994754624'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/266113270994754624'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2006/11/watch-this-space-for-exam-iv.html' title='Watch This Space for Exam IV Information - 2006'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-115591587361540451</id><published>2006-08-18T11:40:00.000-04:00</published><updated>2006-11-15T12:04:43.577-05:00</updated><title type='text'>A Few Class Reminders</title><content type='html'>Go check &lt;a href="http://www.gpc.edu/~jsummero/HistGeol2006.htm"&gt;my Historical webpage&lt;/a&gt;, though not updated, it has Power Point links for each chapter.  The old syllabi are linked there, for references sake, until updates are available.&lt;br /&gt;&lt;br /&gt;Reminder, no class on Monday, 9/4 due to Labor Day Holiday.&lt;br /&gt;&lt;br /&gt;The first lecture will primarily be an introduction to the course.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-115591587361540451?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/115591587361540451/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=115591587361540451' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/115591587361540451'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/115591587361540451'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2006/08/few-class-reminders.html' title='A Few Class Reminders'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-32906434.post-115583777744371422</id><published>2006-08-17T14:00:00.000-04:00</published><updated>2006-11-15T12:04:43.478-05:00</updated><title type='text'>Greetings for the Fall Semester 2006</title><content type='html'>As the format for GPC faculty websites has changed and there is a learning curve, I will post class updates and links here on this blog for the short-term, at least.&lt;br /&gt;&lt;br /&gt;You can check out my other blogs if you wish, once links are posted.  I only ask that if you disagree with political viewpoints, that you do so in a polite, responsible fashion.&lt;br /&gt;&lt;br /&gt;Thanks.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/32906434-115583777744371422?l=gpcgeoblog.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://gpcgeoblog.blogspot.com/feeds/115583777744371422/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=32906434&amp;postID=115583777744371422' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/115583777744371422'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/32906434/posts/default/115583777744371422'/><link rel='alternate' type='text/html' href='http://gpcgeoblog.blogspot.com/2006/08/greetings-for-fall-semester-2006.html' title='Greetings for the Fall Semester 2006'/><author><name>on-the-rocks</name><uri>http://www.blogger.com/profile/06520348177098321049</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><thr:total>0</thr:total></entry></feed>
