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ID:14269268
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页数:14页
时间:2018-07-27
《types of mountains - rutherford county schools:山-卢瑟福县学校类型》由会员上传分享,免费在线阅读,更多相关内容在教育资源-天天文库。
1、TypesofMountains5thGradeTYPESOFMOUNTAINSVolcanic:Folded:Dome:Fault-BlockWithapartner,predicthoweachmountainisformed.TYPESOFMOUNTAINSVolcanic:Shieldandcomposite;magmarisesfromasthenosphereandbreaksthroughthesurfaceofEarthFault-block:normalfaultingandtensionFolded:reversefaultsandcompressionDome:Mag
2、marisesthroughthemantlebutdoesnotbreakthroughthesurface.FoldMountainsFoldmountainsarethemostcommontypeofmountain.Theworld’slargestmountainrangesarefoldmountains.Theserangeswereformedovermillionsofyears.Foldmountainsareformedwhentwoplatescollideheadon,andtheiredgescrumbled,muchthesamewayasapieceofp
3、aperfoldswhenpushedtogether.Theupwardfoldsareknownasanticlines,andthedownwardfoldsaresynclines.Examplesoffoldmountainsinclude:HimalayanMountainsinAsiatheAlpsinEuropetheAndesinSouthAmericatheRockiesinNorthAmericatheUralsinRussiaTheHimalayanMountainswereformedwhenIndiacrashedintoAsiaandpusheduptheta
4、llestmountainrangeonthecontinents.InSouthAmerica,theAndesMountainswereformedbythecollisionoftheSouthAmericancontinentalplateandtheoceanicPacificplate.Fault-BlockThesemountainsformwhenfaultsorcracksintheearth'scrustforcesomematerialsorblocksofrockupandothersdown.Insteadoftheearthfoldingover,theear
5、th'scrustfractures(pullsapart).Itbreaksupintoblocksorchunks.Sometimestheseblocksofrockmoveupanddown,astheymoveapartandblocksofrockendupbeingstackedononeanother.Oftenfault-blockmountainshaveasteepfrontsideandaslopingbackside.Fault-BlockExamplesoffault-blockmountainsinclude:TheSierraNevadamountainsi
6、nNorthAmericaTheHarzMountainsinGermanyDomeDomemountainsaretheresultofagreatamountofmeltedrock(magma)pushingitswayupundertheearthcrust.Withoutactuallyeruptingontothesurface,themagmapushesupoverlayingrocklayers.Atsomepoint,themagmacoolsandformshardenedrock.Theupliftedareacreatedbyrisingmagmaiscalled
7、adomebecauseoflookinglikethetophalfofasphere(ball).Therocklayersoverthehardenedmagmaarewarpedupwardtoformthedome.Buttherocklayersofthesurroundingarearemainflat.Asthedomeishigherthanitssurroundings,erosionbywindan
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