modeling seafloor spreading · modeling seafloor spreading adapted from a lesson developed by san...

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Teacher Instruction Sheet Modeling Seafloor Spreading Adapted from a lesson developed by San Lorenzo USD Teachers: Julie Ramirez, Veenu Soni, Marilyn Stewart, and Lawrence Yano (2012) Teacher Background The process of seafloor spreading created the seafloor of the oceans. For example, in the Atlantic Ocean, North America and South America moved away from Europe and Africa and the resulting crack was filled by mantle material, which cooled and formed new lithosphere. The process continues today. Molten mantle materials continually rise to fill the cracks formed as the plates move slowly apart from each other. This process creates an underwater mountain chain, known as a mid-ocean ridge, along the zone of newly forming seafloor. Molten rock erupts along a mid-ocean ridge, then cools and freezes to become solid rock. The direction of the magnetic field of the Earth at the time the rock cools is "frozen" in place. This happens because magnetic minerals in the molten rock are free to rotate so that they are aligned with the Earth's magnetic field. After the molten rock cools to a solid rock, these minerals can no longer rotate freely. At irregular intervals, averaging about 200-thousand years, the Earth's magnetic field reverses. The end of a compass needle that today points to the north will instead point to the south after the next reversal. The oceanic plates act as a giant tape recorder, preserving in their magnetic minerals the orientation of the magnetic field present at the time of their creation. Geologists call the current orientation "normal" and the opposite orientation "reversed." USGS

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Page 1: Modeling Seafloor Spreading · Modeling Seafloor Spreading Adapted from a lesson developed by San Lorenzo USD Teachers: Julie Ramirez, Veenu Soni, Marilyn Stewart, and Lawrence Yano

Teacher Instruction Sheet

ModelingSeafloorSpreadingAdaptedfromalessondevelopedbySanLorenzoUSDTeachers:JulieRamirez,VeenuSoni,MarilynStewart,andLawrenceYano(2012)TeacherBackgroundTheprocessofseafloorspreadingcreatedtheseaflooroftheoceans.Forexample,intheAtlanticOcean,NorthAmericaandSouthAmericamovedawayfromEuropeandAfricaandtheresultingcrackwasfilledbymantlematerial,whichcooledandformednewlithosphere.Theprocesscontinuestoday.Moltenmantlematerialscontinuallyrisetofillthecracksformedastheplatesmoveslowlyapartfromeachother.Thisprocesscreatesanunderwatermountainchain,knownasamid-oceanridge,alongthezoneofnewlyformingseafloor.Moltenrockeruptsalongamid-oceanridge,thencoolsandfreezestobecomesolidrock.ThedirectionofthemagneticfieldoftheEarthatthetimetherockcoolsis"frozen"inplace.ThishappensbecausemagneticmineralsinthemoltenrockarefreetorotatesothattheyarealignedwiththeEarth'smagneticfield.Afterthemoltenrockcoolstoasolidrock,thesemineralscannolongerrotatefreely.Atirregularintervals,averagingabout200-thousandyears,theEarth'smagneticfieldreverses.Theendofacompassneedlethattodaypointstothenorthwillinsteadpointtothesouthafterthenextreversal.Theoceanicplatesactasagianttaperecorder,preservingintheirmagneticmineralstheorientationofthemagneticfieldpresentatthetimeoftheircreation.Geologistscallthecurrentorientation"normal"andtheoppositeorientation"reversed."

USGS

Page 2: Modeling Seafloor Spreading · Modeling Seafloor Spreading Adapted from a lesson developed by San Lorenzo USD Teachers: Julie Ramirez, Veenu Soni, Marilyn Stewart, and Lawrence Yano

Teacher Instruction Sheet

Inthefigureabove,twoplatesaremovingapart.Amid-oceanridgemarksthelocationwheremoltenmagmaandlavearemovingup,cooling,andformingnewoceanfloor.Thezonesofnormalmagnetizationareindicatedby//////shadingoftheoceaniccrust.Thefigurebelowshowstheobservedmagneticpatternalongthemid-AtlanticRidgesouthofIceland.

Mattox(1992)

Basedonthepatternandspacingoftheoceanicmagneticstripesandtheinferredmotionoftheplates,theageoftheoceanfloorcanbedetermined.Inthefigurebelow,theageoftheoceanfloorisdepicted.

Müllerandothers(1997)

Page 3: Modeling Seafloor Spreading · Modeling Seafloor Spreading Adapted from a lesson developed by San Lorenzo USD Teachers: Julie Ramirez, Veenu Soni, Marilyn Stewart, and Lawrence Yano

Teacher Instruction Sheet

Suggestedtimetocompletethislessonistwo50-minuteperiodsbutmaybeadjustedforalongerclassperiod.

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)QuickWriteAskstudentswhymodelsarenecessaryforstudyingtheEarth?Studentsmayrecordtheirthoughtsonthestudentdatasheet.ManyEarthprocessesoccuroververylargedistancesandoveraverylongperiodsoftime(millionsofyears).ThescaleofEarthprocessesmakesitdifficulttodirectlymeasuretheseprocesses.Wehavelearnedthatscientistsoftenusemodelstoexplaintheirthinking.Wehaveusedglobes,maps,diagrams;chartsetc.whensizeorsafetyissueskeepusfromviewingtherealthing.Sotodaywearegoingtoconsiderhowwemightmakeamodelthatwouldexplainordemonstrateseafloorspreading.ThinkPairShareTurnandtalktoyourelbowpartner:Ifyouweremakingamodelofsea-floorspreading,whataretheimportantideasthatareassociatedwithseafloorspreading?Shareout.Expectedstudentanswers:

•Themid-oceanridge•Symmetricalmagneticpatterns

Page 4: Modeling Seafloor Spreading · Modeling Seafloor Spreading Adapted from a lesson developed by San Lorenzo USD Teachers: Julie Ramirez, Veenu Soni, Marilyn Stewart, and Lawrence Yano

Teacher Instruction Sheet

•AgeofrocksStudentsshouldusethestudentdatasheettorecordtheirthoughts.Youhavecomeupwithsomeimportantideasthatneedtobeincluded.(Ifanypartsaremissing,ask“Whatabout_______________doyouthinkthisshouldbeincluded?”)“TodaywearegoingtocreateamodelthatIhopewillincorporateallofyourimportantpoints.”1.Studentswillmaketheirownmodelsofseafloorspreadingandthemagneticstripsthatoccurin

theseafloor.Havestudentsworkingroupsoffour.

2.Havestudentspickupmaterialsneededfortheactivity.

Materials:

60cmlongpaperstrip 1compass1boxofmarkers 1cardboardboxlid1barmagnet MeterStickorruler

3.Assignjobs:

• StudentA:PaperPuller• StudentB:CompassReader• StudentC:Marker• StudentD:MagnetManager

Thefollowingdirectionshavemanysteps.Sincetheyarepulling,marking,flippingetc.itisrecommendedthattheteacherdemonstratehowtocreatethemodelbyshowingatleast2examplesofmagneticreversals.

4.PaperPuller:Measureandcut60cmofthepaperstrip.Foldthestripinhalflengthwisesoitis

approximately30cmlong.Pushtheendsofthestripthroughtheslitinthelidofacardboardboxsothatitisstickingoutabout5cmonthetopofthelid.Leavethefoldedendofthestripunderneaththebox.

5.Marker:Drawalineinthecenterofthepaper(whereitiscomingoutofthebox)makingsuretomarkbothsidesofthepaper.6.CompassReader:Placethecompassnexttothepaperwhereitiscomingoutofthebox.7.MagnetManager:Placethemagnetontheoppositesideofthepaperfromthecompass.8.CompassReader:ObservewhichdirectionisNorthandtelltheMarker.9.Marker:DrawanarrowpointingNorthonbothsidesofthepaper.Labelthefirstsectiononboth

sideswithan“A”.10.PaperPuller:pulloutsomemorepaper.Marker:drawalineinthecenterofthepaperwhereit

cameoutofthebox.MagnetManager:Flipthemagnetintheoppositedirection.CompassReader:Readthecompass.TelltheMarkertodrawanarrowonpointingtothenewNorthonbothsidesofthepaper.Labelthesecondsectiononbothsidesofthepaperwitha“B”.

11.Repeatstep10untilyoureachtheendofthepaper.MakesurethattheMagnetManagerflipsthemagneteachtime.

Page 5: Modeling Seafloor Spreading · Modeling Seafloor Spreading Adapted from a lesson developed by San Lorenzo USD Teachers: Julie Ramirez, Veenu Soni, Marilyn Stewart, and Lawrence Yano

Teacher Instruction Sheet

LookingatPartsoftheModelHavestudentsrecordtheirideasonthestudentworksheet.1. Whatdoesthepaperstripusedinthemodelrepresentinreallife?Paperstriprepresents

seafloor2. Whenthestripsofpaperarepulledout,whatprocessdoesthisrepresent?Pullingoutthestrips

ofpaperrepresentstheprocessofseafloorspreading3. Whatdoesthemagnetrepresent?ThemagnetrepresentstheEarth’smagneticfield4. Whatdothesectionswitharrowsrepresent?(Whyaretheypointingindifferentdirections)?

ArrowsrepresentthedifferentorientationsoftheEarth’smagneticfieldwhentheseafloorformed.

5. Whatdothedifferentsectionsofthepaperstrip(A,B,C,etc.)represent?Thedifferentsectionsrepresentthemagneticstripesintheseafloor

6. Inthemodel,whatdoesflippingthemagnetrepresent?FlippingthemagnetrepresentstheEarth’smagneticreversals

7. Didweincludealltheimportantelementsneededtoexplainseafloorspreading?Ifyes,whatarethey?Ifno,whatismissing?

8. Canyouthinkofawaythatwecouldadd/delete/changeitemsthatwouldmakethismodelmoreeffective?

9. CanyouthinkofawaythatwecouldusethismodeltoexplainWegener’sideaofContinentalDrift?

ExitTicketInthespacebelow,drawadiagramofseafloorspreading.Includeasmuchdetailasyoucan. Vocabularywords–keyvocabularywordsthataretargetedortaughtaspartofthelesson.(Understandingthesewordsisessentialforstudentstounderstandthekeyconceptsofthislesson.)Seafloor MagnetMagneticField Mid-oceanRidge PotentialPitfalls• Studentsshouldunderstandthattherearenotvisiblestripesontheseafloor.Magneticstripesin

diagramsportraytheorientationofthemagneticfieldthatismeasuredbyscientificinstrumentsthatarepreservedintherocksandarenotvisible.

• Spreadingatmid-oceanridgesisnotacontinuousprocess(likeaconveyerbelt)butoccursinepisodes.