* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Modeling Seafloor Spreading
Survey
Document related concepts
Transcript
Teacher Instruction Sheet ModelingSeafloorSpreading AdaptedfromalessondevelopedbySanLorenzoUSDTeachers:JulieRamirez,VeenuSoni,MarilynStewart,and LawrenceYano(2012) TeacherBackground Theprocessofseafloorspreadingcreatedtheseaflooroftheoceans.Forexample,intheAtlantic Ocean,NorthAmericaandSouthAmericamovedawayfromEuropeandAfricaandtheresultingcrack wasfilledbymantlematerial,whichcooledandformednewlithosphere.Theprocesscontinuestoday. Moltenmantlematerialscontinuallyrisetofillthecracksformedastheplatesmoveslowlyapartfrom eachother.Thisprocesscreatesanunderwatermountainchain,knownasamid-oceanridge,alongthe zoneofnewlyformingseafloor. Moltenrockeruptsalongamid-oceanridge,thencoolsandfreezestobecomesolidrock.Thedirection ofthemagneticfieldoftheEarthatthetimetherockcoolsis"frozen"inplace.Thishappensbecause magneticmineralsinthemoltenrockarefreetorotatesothattheyarealignedwiththeEarth's magneticfield.Afterthemoltenrockcoolstoasolidrock,thesemineralscannolongerrotatefreely.At irregularintervals,averagingabout200-thousandyears,theEarth'smagneticfieldreverses.Theendofa compassneedlethattodaypointstothenorthwillinsteadpointtothesouthafterthenextreversal. Theoceanicplatesactasagianttaperecorder,preservingintheirmagneticmineralstheorientationof themagneticfieldpresentatthetimeoftheircreation.Geologistscallthecurrentorientation"normal" andtheoppositeorientation"reversed." USGS Teacher Instruction Sheet Inthefigureabove,twoplatesaremovingapart.Amid-oceanridgemarksthelocationwheremolten magmaandlavearemovingup,cooling,andformingnewoceanfloor.Thezonesofnormal magnetizationareindicatedby//////shadingoftheoceaniccrust. Thefigurebelowshowstheobservedmagneticpatternalongthemid-AtlanticRidgesouthofIceland. Mattox(1992) Basedonthepatternandspacingoftheoceanicmagneticstripesandtheinferredmotionoftheplates, theageoftheoceanfloorcanbedetermined.Inthefigurebelow,theageoftheoceanfloorisdepicted. Müllerandothers(1997) Teacher Instruction Sheet Suggestedtimetocompletethislessonistwo50-minuteperiodsbutmaybeadjustedforalonger classperiod. DAY1 • ShowavideoaboutHaroldHessandhisdiscoveries. https://www.youtube.com/watch?v=GyMLlLxbfa4 • AskstudentstotalktotheirelbowpartneranddiscusswitheachotherwhoWegenerwas.Have studentscalloutwhattheyrememberabouthisdiscoveries. • AskstudentshowWegenermusthavefeltwhenpeopledidnotsupporthisideaabout ContinentalDrift? • WhydidthescientificcommunityinitiallydismissWegner’sideaaboutContinentalDrift? • Whatdidotherscientistshaveissueswith? • HowdoHess’discoveriesrelatetowhatWegener’sContinentalDrift? DAY2 • Studentsmayneedclarificationaboutthemagneticpolereversals. • Usea“StericDemonstratorofMagneticLine–of-Force”modeltoshowtheexistenceofthe magneticfieldsandthespatialdistributionofmagneticlinesofforce. • “YesterdaywetalkedaboutHarryHessandhistheoryofseafloorspreading.Whatimportant discoveriesdidHessandhisfellowscientistsmake?“ ExpectedStudentResponses • Continuouschainofunderseamountainsknownasthemid-oceanridge • Symmetricalpatternsofmagneticreversalsshownbymetalcrystalsembeddedinrocks • Rocksthatwerefartherawayfromridgewereolder(ageofrocks) QuickWrite AskstudentswhymodelsarenecessaryforstudyingtheEarth?Studentsmayrecordtheirthoughts onthestudentdatasheet. ManyEarthprocessesoccuroververylargedistancesandoveraverylongperiodsoftime(millions ofyears).ThescaleofEarthprocessesmakesitdifficulttodirectlymeasuretheseprocesses.We havelearnedthatscientistsoftenusemodelstoexplaintheirthinking.Wehaveusedglobes,maps, diagrams;chartsetc.whensizeorsafetyissueskeepusfromviewingtherealthing.Sotodayweare goingtoconsiderhowwemightmakeamodelthatwouldexplainordemonstrateseafloor spreading. ThinkPairShare Turnandtalktoyourelbowpartner:Ifyouweremakingamodelofsea-floorspreading,whatarethe importantideasthatareassociatedwithseafloorspreading?Shareout. Expectedstudentanswers: •Themid-oceanridge •Symmetricalmagneticpatterns Teacher Instruction Sheet •Ageofrocks Studentsshouldusethestudentdatasheettorecordtheirthoughts. Youhavecomeupwithsomeimportantideasthatneedtobeincluded.(Ifanypartsaremissing,ask “Whatabout_______________doyouthinkthisshouldbeincluded?”) “TodaywearegoingtocreateamodelthatIhopewillincorporateallofyourimportantpoints.” 1.Studentswillmaketheirownmodelsofseafloorspreadingandthemagneticstripsthatoccurin theseafloor.Havestudentsworkingroupsoffour. 2.Havestudentspickupmaterialsneededfortheactivity. Materials: 60cmlongpaperstrip 1boxofmarkers 1barmagnet 1compass 1cardboardboxlid MeterStickorruler 3.Assignjobs: • StudentA:PaperPuller • StudentB:CompassReader • StudentC:Marker • StudentD:MagnetManager Thefollowingdirectionshavemanysteps.Sincetheyarepulling,marking,flippingetc.itis recommendedthattheteacherdemonstratehowtocreatethemodelbyshowingatleast2 examplesofmagneticreversals. 4.PaperPuller:Measureandcut60cmofthepaperstrip.Foldthestripinhalflengthwisesoitis approximately30cmlong.Pushtheendsofthestripthroughtheslitinthelidofacardboardbox sothatitisstickingoutabout5cmonthetopofthelid.Leavethefoldedendofthestrip underneaththebox. 5.Marker:Drawalineinthecenterofthepaper(whereitiscomingoutofthebox)makingsureto markbothsidesofthepaper. 6.CompassReader:Placethecompassnexttothepaperwhereitiscomingoutofthebox. 7.MagnetManager:Placethemagnetontheoppositesideofthepaperfromthecompass. 8.CompassReader:ObservewhichdirectionisNorthandtelltheMarker. 9.Marker:DrawanarrowpointingNorthonbothsidesofthepaper.Labelthefirstsectiononboth sideswithan“A”. 10.PaperPuller:pulloutsomemorepaper.Marker:drawalineinthecenterofthepaperwhereit cameoutofthebox.MagnetManager:Flipthemagnetintheoppositedirection.Compass Reader:Readthecompass.TelltheMarkertodrawanarrowonpointingtothenewNorthon bothsidesofthepaper.Labelthesecondsectiononbothsidesofthepaperwitha“B”. 11.Repeatstep10untilyoureachtheendofthepaper.MakesurethattheMagnetManagerflips themagneteachtime. Teacher Instruction Sheet LookingatPartsoftheModel Havestudentsrecordtheirideasonthestudentworksheet. 1. Whatdoesthepaperstripusedinthemodelrepresentinreallife?Paperstriprepresents seafloor 2. Whenthestripsofpaperarepulledout,whatprocessdoesthisrepresent?Pullingoutthestrips ofpaperrepresentstheprocessofseafloorspreading 3. Whatdoesthemagnetrepresent?ThemagnetrepresentstheEarth’smagneticfield 4. Whatdothesectionswitharrowsrepresent?(Whyaretheypointingindifferentdirections)? ArrowsrepresentthedifferentorientationsoftheEarth’smagneticfieldwhentheseafloor formed. 5. Whatdothedifferentsectionsofthepaperstrip(A,B,C,etc.)represent?Thedifferentsections representthemagneticstripesintheseafloor 6. Inthemodel,whatdoesflippingthemagnetrepresent?Flippingthemagnetrepresentsthe Earth’smagneticreversals 7. Didweincludealltheimportantelementsneededtoexplainseafloorspreading?Ifyes,whatare they?Ifno,whatismissing? 8. Canyouthinkofawaythatwecouldadd/delete/changeitemsthatwouldmakethismodelmore effective? 9. CanyouthinkofawaythatwecouldusethismodeltoexplainWegener’sideaofContinental Drift? ExitTicketInthespacebelow,drawadiagramofseafloorspreading.Includeasmuchdetailasyoucan. Vocabularywords–keyvocabularywordsthataretargetedortaughtaspartofthelesson. (Understandingthesewordsisessentialforstudentstounderstandthekeyconceptsofthislesson.) Seafloor MagnetMagneticField Mid-oceanRidge PotentialPitfalls • Studentsshouldunderstandthattherearenotvisiblestripesontheseafloor.Magneticstripesin diagramsportraytheorientationofthemagneticfieldthatismeasuredbyscientificinstruments thatarepreservedintherocksandarenotvisible. • Spreadingatmid-oceanridgesisnotacontinuousprocess(likeaconveyerbelt)butoccursin episodes.