托福在线阅读最新.docx
- 文档编号:23764594
- 上传时间:2023-05-20
- 格式:DOCX
- 页数:24
- 大小:25.83KB
托福在线阅读最新.docx
《托福在线阅读最新.docx》由会员分享,可在线阅读,更多相关《托福在线阅读最新.docx(24页珍藏版)》请在冰豆网上搜索。
托福在线阅读最新
TheSurfaceofMars
Paragraph1
ThesurfaceofMarsshowsawiderangeofgeologicfeatures,includinghugevolcanoes-thelargestknowninthesolarsystem-andextensiveimpactcratering.ThreeverylargevolcanoesarefoundontheTharsisbulge,anenormousgeologicareanearMars'sequator.NorthwestofTharsisisthelargestvolcanoofall:
OlympusMons,withaheightof25kilometersandmeasuringsome700kilometersindiameteratitsbase.ThethreelargevolcanoesontheTharsisbulgearealittlesmaller-a"mere"18kilometershigh.
Paragraph2
NoneofthesevolcanoeswasformedasaresultofcollisionsbetweenplatesoftheMartiancrust-thereisnoplatemotiononMars.Instead,theyareshieldvolcanoes-volcanoeswithbroad,slopingslidesformedbymoltenrock.AllfourshowdistinctivelavachannelsandotherflowfeaturessimilartothosefoundonshieldvolcanoesonEarth.ImagesoftheMartiansurfacerevealmanyhundredsofvolcanoes.MostofthelargestvolcanoesareassociatedwiththeTharsisbulge,butmanysmalleronesarefoundinthenorthernplains.
Paragraph3
ThegreatheightofMartianvolcanoesisadirectconsequenceoftheplanet'slowsurfacegravity.Aslavaflowsandspreadstoformashieldvolcano,thevolcano'seventualheightdependsonthenewmountain'sabilitytosupportitsownweight.Thelowerthegravity,thelessertheweightandthegreatertheheightofthemountain.ItisnoaccidentthatMaxwellMonsonVenusandtheHawaiianshieldvolcanoesonEarthrisetoaboutthesameheight(about10kilometers)abovetheirrespectivebases-EarthandVenushavesimilarsurfacegravity.Mars'ssurfacegravityisonly40percentthatofEarth,sovolcanoesriseroughly2.5timesashigh.AretheMartianshieldvolcanoesstillactive?
Scientistshavenodirectevidenceforrecentorongoingeruptions,butifthesevolcanoeswereactiveasrecentlyas100million,yearsago(anestimateofthetimeoflast"eruptionbasedontheextentofimpactcrateringontheirslopes),someofthemmaystillbeatleastintermittentlyactive.Millionsofyears,though,maypassbetweeneruptions.
Paragraph4
AnotherprominentfeatureofMars'ssurfaceiscratering.TheMarinerspacecraftfoundthatthesurfaceofMars,aswellasthatofitstwomoons,ispittedwithimpactcratersformedbymeteoroidsfallinginfromspace.AsonourMoon,thesmallercratersareoftenfilledwithsurfacematter-mostlydust-confirmingthatMarsisadrydesertworld.However,Martiancratersgetfilledinconsiderablyfasterthantheirlunarcounterparts.OntheMoon,ancientcraterslessthan100metersacross(correspondingtodepthsofabout20meters)havebeenobliterated,primarilybymeteoriticerosion.OnMars,therearerelativelyfewcraterslessthan5kilometersindiameter.TheMartianatmosphereisanefficienterosiveagent,withMartianwindstransportingdustfromplacetoplaceanderasingsurfacefeaturesmuchfasterthanmeteoriticimpactsalonecanobliteratethem.
Paragraph5
AsontheMoon,theextentoflargeimpactcratering(i.e.craterstoobigtohavebeenfilledinbyerosionsincetheywereformed)servesasanageindicatorfortheMartiansurface.AgeestimatesrangingfromfourbillionyearsforMars'ssouthernhighlandstoafewhundredmillionyearsintheyoungestvolcanicareaswereobtainedinthisway.
Paragraph6
ThedetailedappearanceofMartianimpactcratersprovidesanimportantpieceofinformationaboutconditionsjustbelowtheplanet'ssurface.Martiancratersaresurroundedbyejecta(debrisformedasaresultofanimpact)thatlooksquitedifferentfromitslunarcounterparts.AcomparisonoftheCopernicuscraterontheMoonwiththe(fairlytypical)craterYutyonMarsdemonstratesthedifferences.Theejectasurroundingthelunarcraterisjustwhatonewouldexpectfromanexplosionejectingalargevolumeofdust,soil,andboulders.However,theejectaonMarsgivesthedistinctimpressionofaliquidthathassplashedorflowedoutofcrater.Geologiststhinkthatthisfluidizedejectacraterindicatesthatalayerofpermafrost,orwaterice,liesjustafewmetersunderthesurface.Explosiveimpactsheatedandliquefiedtheice,resultinginthefluidappearanceoftheejecta.
Paragraph1
ThesurfaceofMarsshowsawiderangeofgeologicfeatures,includinghugevolcanoes-thelargestknowninthesolarsystem-andextensiveimpactcratering.ThreeverylargevolcanoesarefoundontheTharsisbulge,anenormousgeologicareanearMars'sequator.NorthwestofTharsisisthelargestvolcanoofall:
OlympusMons,withaheightof25kilometersandmeasuringsome700kilometersindiameteratitsbase.ThethreelargevolcanoesontheTharsisbulgearealittlesmaller-a"mere"18kilometershigh.
1、Theword"enormous"Inthepassageisclosestinmeaningto
○Important
○Extremelylarge
○Highlyunusual
○Active
2、Accordingtoparagraph1,OlympusMonsdiffersfromvolcanoesontheTharsisbulgeinthatOlympus
Mons
○Hasmorecomplexgeologicfeatures
○Showslessimpactcratenng
○istaller
○Wasformedatalatertime
Paragraph2
NoneofthesevolcanoeswasformedasaresultofcollisionsbetweenplatesoftheMartiancrust-thereisnoplatemotiononMars.Instead,theyareshieldvolcanoes-volcanoeswithbroad,slopingslidesformedbymoltenrock.AllfourshowdistinctivelavachannelsandotherflowfeaturessimilartothosefoundonshieldvolcanoesonEarth.ImagesoftheMartiansurfacerevealmanyhundredsofvolcanoes.MostofthelargestvolcanoesareassociatedwiththeTharsisbulge,butmanysmalleronesarefoundinthenorthernplains.
3、Theword"distinctive”inthepassageisclosestinmeaningto
○Deep
○Complex
○Characteristic
○Ancient
4、Accordingtoparagraphs1and2,whichofthefollowingisNOTtrueoftheshieldvolcanoesontheTharsisbulge?
Theyhavebroad,slopingsides.
TheyaresmallerthanthelargestvolcanoonMars.
TheyhavechannelsthatresemblethelavachannelsofvolcanoesonEarth.
Theyareover25kilometerstall.
Paragraph3
ThegreatheightofMartianvolcanoesisadirectconsequenceoftheplanet'slowsurfacegravity.Aslavaflowsandspreadstoformashieldvolcano,thevolcano'seventualheightdependsonthenewmountain'sabilitytosupportitsownweight.Thelowerthegravity,thelessertheweightandthegreatertheheightofthemountain.ItisnoaccidentthatMaxwellMonsonVenusandtheHawaiianshieldvolcanoesonEarthrisetoaboutthesameheight(about10kilometers)abovetheirrespectivebases-EarthandVenushavesimilarsurfacegravity.Mars'ssurfacegravityisonly40percentthatofEarth,sovolcanoesriseroughly2.5timesashigh.AretheMartianshieldvolcanoesstillactive?
Scientistshavenodirectevidenceforrecentorongoingeruptions,butifthesevolcanoeswereactiveasrecentlyas100million,yearsago(anestimateofthetimeoflast"eruptionbasedontheextentofimpactcrateringontheirslopes),someofthemmaystillbeatleastintermittentlyactive.Millionsofyears,though,maypassbetweeneruptions.
5、Theword"roughly"closestInmeaningto
Typically
Frequently
Actually
Approximately
6、Inparagraph3,whydoestheauthorcompareMaxwellMonsonVenustotheHawaiianshieldvolcanoesonEarth?
Tohelpexplaintherelationshipbetweensurfacegravityandvolcanoheight
ToexplainwhyMars'ssurfacegravityisonly40percentofEarth's
TopointoutdifferencesbetweenthesurfacegravityofEarthandthesurfacegravityofVenus
Toarguethattherearemoresimilaritiesthandifferencesbetweenvolcanoesondifferentplanets
7、Whichofthesentencesbelowbestexpressestheessentialinformationinthehighlightedsentenceinthepassage?
Incorrectchoiceschangethemeaninginimportantwaysorleaveoutessentialinformation.
Althoughdirectevidenceofrecenteruptionsislacking,scientistsbelievethatthesevolcanoeswereactiveasrecentlyas100millionyearsago.
Scientistsestimatethatvolcanoesactivemorerecentlythan100yearsagowillstillhaveextensiveimpactcrateringontheirslopes.
If,assomeevidencesuggests,thesevolcanoeseruptedasrecentlyas100millionyearsago,theymaycontinuetobeintermittentlyactive.
Althoughthesevolcanoeswereactiveasrecentlyas100millionyearsago,thereisnodirectevidenceofrecentorongoingeruptions.
Paragraph4
AnotherprominentfeatureofMars'ssurfaceiscratering.TheMarinerspacecraftfoundthatthesurfaceofMars,aswellasthatofitstwomoons,ispittedwithimpactcratersformedbymeteoroidsfallinginfromspace.AsonourMoon,thesmallercratersareoftenfilledwithsurfacematter-mostlydust-confirmingthatMarsisadrydesertworld.However,Martiancratersgetfilledinconsiderablyfasterthantheirlunarcounterparts.OntheMoon,ancientcraterslessthan100metersacross(correspondingtodepthsofabout20meters)havebeenobliterated,primarilybymeteoriticerosion.OnMars,therearerelativelyfewcraterslessthan5kilometersindiameter.TheMartianatmosphereisanefficienterosiveagent,withMartianwindstransportingdustfromplacetoplaceanderasingsurfacefeaturesmuchfasterthanmeteoriticimpactsalonecanobliteratethem.
8、Theword"considerably"inthepassageisclosestinmeaningto
Frequently
Significantly
Clearly
Surprisingly
9、Accordingtoparagraph4,whatisdemonstratedbythefactthatcratersfillinmuchfasteronMarsthanontheMoon?
ErosionfrommeteoriticimpactstakesplacemorequicklyonMarsthanontheMoon.
ThereismoredustonMarsthanontheMoon.
ThesurfaceofMarsisadrydesert.
WindisapowerfulerodingforceonMars.
10、Inthepapragraph4,whydoestheauthorpointoutthatMarshasfewancientcratersthatar
- 配套讲稿:
如PPT文件的首页显示word图标,表示该PPT已包含配套word讲稿。双击word图标可打开word文档。
- 特殊限制:
部分文档作品中含有的国旗、国徽等图片,仅作为作品整体效果示例展示,禁止商用。设计者仅对作品中独创性部分享有著作权。
- 关 键 词:
- 托福 在线 阅读 最新