Geomorphology Weekly Notes 5-2.htm
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<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 3.2 Final//EN"> <!-- Created from PDF via Acrobat SaveAsXML --> <!-- Mapping table version: 28-February-2003 --> <HTML> <HEAD> <META name="dc.title" content=" " > <META name="dc.date" content="2009-08-13T11:19:14-04:00" > <META name="dc.date.modified" content="2009-08-13T11:19:18-04:00" > <META name="generator" content="Adobe Acrobat Exchange-Pro 7.8" > </HEAD> <BODY bgcolor=white text=black link=blue vlink=purple alink=fushia > <DIV class="Sect" ><DIV ><P align="justify" ><IMG width="85" height="72" src="images/Geomorphology Weekly Notes 5-2_img_0.jpg" ></P ></DIV ><DIV ><P align="justify" ><IMG width="43" height="68" src="images/Geomorphology Weekly Notes 5-2_img_1.jpg" ></P ></DIV ><DIV ><P align="justify" ><FONT size="+1" color="#000000"></B>Desert & Poles vs. tropic<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Iron sulfide of marsh and swamp<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Hydrolysis- Weak acid Si02 Dissolved in h2o (H4Si04)<FONT size="+1"> </P ></DIV ><DIV ><P align="justify" ><FONT size="+1">(Much more C02 in soil than air and in ocean also) <FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Hydrolysis of feldspars (orthoclase & plagioclase) 50% of earth's minerals<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Clay and aluminum silicates - Bauxite<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Kaolin, vermiculite, chlorite, montmonorillite<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Weathering series of rocks- millions to less than 200 years.<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Microbial, weathering, algae, fungi, Cyanobacteria to clean up chemical wastes.<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Review soil horizons<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">0-A-B-C <FONT size="+1"> </P ><P align="justify" > <FONT size="+1"> A B C<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Karst - solution topography<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">High rock solubility & porocity<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Solution is weathering and erosion combined<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Dolomite & gypsum salt increases<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Tropics to Poles<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Karstology & terminology<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Hypogenic Caves (sulfuric acid)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">CaCo3 epigenic / near surface<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">H20 + HC03 carbonic acid<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Pressure, mixing, temp (different types of h2o)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Phytokarst of Grand Canyan - cyanobacteria<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Guano - Chincha Islands - Rock Phosphate<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Nauru and Ocean is in pacific<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Cold Water vs. Warm Water<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Cave use historically- Caves & bandits from Jesse James to V C to Julio 14 to Chetniks<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Cause - deep flow paths below water table and in areas of water table fluctuation<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Caves are horizontal & support<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Speleotherms - Stalactites vs. Stalagmites<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Cols and submerged Pools<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Mass Wasting - Weathered Rock<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Gravity, pressure, flowing h2o<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Angle of Repose gp - gt<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Gt greater than gp- Than rock moves down hill<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Cohesion - from ground - (40-60%h2o)<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Slope - 25 - 40 - movement - depends upon type<FONT size="+1"> </P ><P align="justify" ><FONT size="+1">Description - Fall, rock, debris, earth, monolith fall<FONT size="+1"> </P ></DIV ></DIV ></BODY> </HTML>
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rsadoo. (Aug 17, 2009). Geomorphology Weekly Notes 5-2.htm. Retrieved Nov 06, 2014, from UMass Boston OpenCourseware Web site: http://ocw.umb.edu/environmental-earth-and-ocean-sciences/eeos-302-geomorphology/Geomorphology%20Weekly%20Notes%205-2.htm.