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PAGE\*MERGEFORMAT6 托福阅读真题集锦(七) PASSAGE13 Anyrockthathascooledandsolidifiedfromamoltenstateisanigneousrock.Therefore,iftheEarthbeganasasuperheatedsphereinspace,alltherocksmakingupitscrustmaywellhavebeenigneousandthustheancestorsofallotherrocks.Eventoday,approximately95percentoftheentirecrustisigneous.Periodically,moltenmaterialwellsoutoftheEarth'sinteriortoinvadethesurfacelayersortoflowontothesurfaceitself.Thismaterialcoolsintoawidevarietyofigneousrocks.Inthemoltenstate,itiscalledmagmaasitpushesintothecrustandlavawhenitrunsoutontothesurface. Allmagmaconsistsbasicallyofavarietyofsilicateminerals(highinsilicon-oxygencompounds),butthechemicalcompositionofanygivenflowmaydifferradicallyfromthatofanyother.Theresultingigneousrockswillreflectthesedifferences.Igneousrocksalsovaryintextureaswellaschemistry.Granite,forinstance,isacoarse-grainedigneousrockwhoseindividualmineralcrystalshaveformedtoasizeeasilyseenbythenakedeye.Aslowrateofcoolinghasallowedthecrystalstoreachthissize.Normally,slowcoolingoccurswhenthecrustisinvadedbymagmathatremainsburiedwellbelowthesurface.Granitemaybefoundonthesurfaceofthecontemporarylandscape,butfromitscoarsetextureweknowthatitmusthaveformedthroughslowcoolingatagreatdepthandlaterbeenlaidbarebyerosion.Igneousrockswiththiscoarse-grainedtexturethatformedatdeptharecalledplutonic. Ontheotherhand,ifthesamemagmaflowsontothesurfaceandisquicklycooledbytheatmosphere,theresultingrockwillbefine-grainedandappearquitedifferentfromgranite,althoughthechemicalcompositionwillbeidentical.Thiskindofrockiscalledrhyolite.Themostfinelygrainedigneousrockisvolcanicglassorobsidian,whichhasnocrystals.Someresearchersbelievethisisbecauseofrapidcooling;othersbelieveitisbecauseofalackofwatervaporandothergasesinthelava.TheblackobsidiancliffsofYellowstoneNationalParkaretheresultofalavaflowofbasaltrunningheadonintoaglacier.Someoftheglaciermeltedoncontact,butsuddenlytherealsoappearedahugeblackmassofglassystone. 1.Inthefirstparagraph,theauthormentionsthat95%oftheEarth'scrusti

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