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Environmental Problems, Their Causes, and Sustainability 1

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usually rides up over the denser oceanic plate <strong>and</strong>pushes it down into the mantle in a process calledsubduction. The area where this collision <strong>and</strong> subductiontakes place is called a subduction zone. Overtime the subducted plate melts <strong>and</strong> rises back to theearth’s surface as molten rock or magma. A trenchordinarily forms at the boundary between the twoconverging plates. Stresses in the plate undergoingsubduction cause earthquakes at convergent plateboundaries.The third type of boundary is a transform fault,which occurs where plates slide <strong>and</strong> grind past one anotheralong a fracture (fault) in the lithosphere (Figure16-5, bottom). Most transform faults are on theocean floor but a few are found on l<strong>and</strong>. An exampleis the North American Plate <strong>and</strong> the Pacific Plate thatslide <strong>and</strong> rub past each other along California’s SanAndreas Fault. As a result, southern California isslowly moving along this transform fault towardnorthern California. Sometime perhaps 30 millionyears from now the geographical area we now call LosAngeles will probably slowly grind <strong>and</strong> slide by thegeographical area now known as San Francisco. But bythen neither of these areas will exist as we know themtoday. This is fascinating stuff from a geological perspectiveof the earth’s history but is not a problem thatwe need worry about.What Geologic Processes Occuron the Earth’s Surface? Erosion <strong>and</strong>WeatheringWater <strong>and</strong> wind move large amounts of soil <strong>and</strong>broken-down pieces of rock from one place toanother.Geologic changes based directly or indirectly on energyfrom the sun <strong>and</strong> on gravity (rather than on heatin the earth’s interior) are called external processes. Internalprocesses generally build up the earth’s surface.In contrast, external processes tend to wear it down<strong>and</strong> produce a variety of l<strong>and</strong>forms <strong>and</strong> environmentsformed by the buildup of eroded sediment.A major external process is erosion: the process bywhich material is dissolved, loosened, or worn awayfrom one part of the earth’s surface <strong>and</strong> deposited elsewhere.Flowing streams cause most erosion. WindEURASIAN PLATEMid-IndianOceanRidgeCHINASUBPLATEINDIAN-AUSTRALIAN PLATEPHILIPPINEPLATETransformfaultJUAN DEFUCA PLATEPACIFICPLATETransformfaultCOCOSPLATEEast PacificRiseNORTHAMERICANPLATENAZCAPLATECARIBBEANPLATEMid-AtlanticOceanRidgeSOUTHAMERICANPLATEReykjanesRidgeANATOLIAN PLATEARABIANPLATEAFRICANPLATESOMALIANSUBPLATEEURASIANPLATECarlsbergRidgeSoutheast IndianOcean RidgeTransformfaultSouthwest IndianOcean RidgeANTARCTIC PLATEConvergentplate boundariesPlate motionat convergentplate boundariesDivergent ( ) <strong>and</strong>transform fault ( )boundariesPlate motionat divergentplate boundariesFigure 16-4 The earth’s major tectonic plates. These b<strong>and</strong>s correspond to the patterns for the types of lithosphericplate boundaries shown in Figure 16-5. What plate do you live on?http://biology.brookscole.com/miller14335

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