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托福阅读――地质地貌类(一).pdf

托福阅读――地质地貌类(一).pdf

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智课网托福备考资料
托福阅读――地质地貌类(一)

ThesurfaceofMars
ThesurfaceofMarsshowsawiderangeofgeologicfeatures,
includinghugevolcanoes-thelargestknowninthesolar
system-andextensiveimpactcratering.Threeverylarge
volcanoesarefoundontheTharsisbulge,anenormousgeologic
areanearMars’sequator.NorthwestofTharsisisthelargest
volcanoofall:OlympusMons,withaheightof25kilometersand
measuringsome700kilometersindiameteratitsbase.Thethree
largevolcanoesontheTharsisbulgearealittlesmaller-a
“mere”18kilometershigh.
Noneofthesevolcanoeswasformedasaresultofcollisions
betweenplatesoftheMartiancrust-thereisnoplatemotionon
Mars.Instead,theyareshieldvolcanoes—volcanoeswithbroad,
slopingslidesformedbymoltenrock.Allfourshowdistinctive
lavachannelsandotherflowfeaturessimilartothosefoundon
shieldvolcanoesonEarth.ImagesoftheMartiansurfacereveal
manyhundredsofvolcanoes.Mostofthelargestvolcanoesare
associatedwiththeTharsisbulge,butmanysmalleronesare
foundinthenorthernplains.
ThegreatheightofMartianvolcanoesisadirect
consequenceoftheplanet’slowsurfacegravity.Aslavaflows
andspreadstoformashieldvolcano,thevolcano’seventual
heightdependsonthenewmountain’sabilitytosupportits
ownweight.Thelowerthegravity,thelessertheweightandthe
greatertheheightofthemountain.ItisnoaccidentthatMaxwell
MonsonVenusandtheHawaiianshieldvolcanoesonEarthrise
toaboutthesameheight(about10kilometers)abovetheir
respectivebases-EarthandVenushavesimilarsurfacegravity.
Mars’ssurfacegravityisonly40percentthatofEarth,so
volcanoesriseroughly2.5timesashigh.AretheMartianshield
volcanoesstillactive?Scientistshavenodirectevidencefor
recentorongoingeruptions,butifthesevolcanoeswereactive
asrecentlyas100millionyearsago(anestimateofthetimeof
lasteruptionbasedontheextentofimpactcrateringontheir
slopes),someofthemmaystillbeatleastintermittentlyactive.
Millionsofyears,though,maypassbetweeneruptions.
AnotherprominentfeatureofMars’ssurfaceiscratering.
TheMarinerspacecraftfoundthatthesurfaceofMars,aswellas
thatofitstwomoons,ispittedwithimpactcratersformedby
meteoro
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