main | welcome to mcla - earth’s surface...student learning targets “i can” statements 1. i...
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TheEvolutionoftheT2LScienceCurriculumOverthelastfouryears,theTeachtoLearnprogramcreated20NGSS-alignedscienceunitsingradesK-5duringoursummersessions.Truetoourplan,wepilotedtheunitsinNorthAdamsPublicSchools,andaskedandreceivedfeedbackfromoursciencefellowsandourparticipatingteachers.Thisfeedbackservedasastartingpointforourrevisionsoftheunits.Duringyear2(Summerof2015),werevisedunitsfromyear1(Summer/Fall2014)andcreatednewunitstopilot.Inyear3,werevisedunitsfromyears1and2andcreatednewunitsofcurricula,usingthesamemodelforyear4.Ourunderstandingofhowtocreaterichandrobustsciencecurriculumgrew,sobythesummerof2018,ourfinalsummerofcurriculumdevelopment,wehadcreatedfiveexemplarunitsandestablishedanexemplarunittemplatewhichisavailableintheT2LToolkit.Wemadeaconcertedefforttoupgradealltheexistingunitswithexemplarcomponents.Wewereabletodomuch,butnotall.So,asyouexploredifferentunits,youwillnoticethatsomecontainallelementsofourexemplarunits,whileotherscontainonlysome.Thefullyrealizedexemplarunitsarenotedonthecoverpage.Wedidreviseall20unitsandbroughtthemtoabaselineof“exemplar”byincludingtheLessons-At-A-GlanceandScienceTalkelements.
T2LCurriculumUnit
Grade4 Earth’s
Surface
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TheEarth’sSurface
EarthScience/Grade4
Inthisunit,studentsinvestigatetheprocessesoferosionandweatheringthroughhands-oninvestigations.Theywillseehowtheseprocessesaffecttheformationoflandforms.Studentswillanalyzedifferenttypesofmapstolookforpatternsandwilldesignasolutiontomitigatetheeffectsofanearthquake.
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UnitCreationandRevisionHistoryAuthorsTiffinieAlvarez,SecondaryEducationmajor,Englishmajor,MassachusettsCollegeofLiberalArts(Summer’18)KathyAtwood,Grade3Teacher,NorthAdamsPublicSchools(Summer‘14)JeanBacon,AdministratorforTeachingandLearning,NorthAdamsPublicSchools(Summer‘14)AminaDiop,Astrophysicsmajor,Mathematicsmajor,WilliamsCollege(Summer‘18)LaurenMangiardi,ElementaryEducationMajor,EnglishLiterature,MassachusettsCollegeofLiberalArts(Summer‘18)PriscillaMercado,Computersciencemajor,Englishmajor,WilliamsCollege(Summer‘18)StephanieNguyen,ElementaryEducationmajor,InterdisciplinaryStudiesmajor,MassachusettsCollegeofLiberalArts(Summer‘18)LindsayOsterhoudt,ScienceCoordinator,NorthAdamsPublicSchools(Summer‘14)MatthewRoychowdhury,Physicsmajor,WilliamsCollege(Summer‘18)TroySegala,BusinessAdministrationManagementmajor,MassachusettsCollegeofLiberalArts(Summer‘14)Revisions,Summer2015JessicaL.Wojcik,InterdisciplinaryStudiesmajor,Educationmajor,SocialWorkminor,MassachusettsCollegeofLiberalArtsGraceSullivan,EnglishandWomen’sStudiesmajor,WilliamsCollegeRevisions,Summer2016DiegoGarcia,ComputerSciencemajor,WilliamsCollegeAnnieGagnon,Biologymajor,MassachusettsCollegeofLiberalArtsProjectManager:LeslieRule,TeachtoLearn,MassachusettsCollegeofLiberalArts
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License/CopyrightInformation
ThiscurriculumunitislicensedundertheCreativeCommonsAttribution-NonCommercial-ShareAlike3.0.(CCBY-NC-SA3.0)
Pleaseseethefulltextofthislicense(http://creativecommons.org/licenses/by-nc-sa/3.0/)toviewallrightsandrestrictionsassociatedwithit.ThisunitwasdevelopedwithfundingfromtheNationalScienceFoundationDOE-IUSEAwardNo.1432591Thisunitisdownloadableathttp://mcla.edu/About_MCLA/area/Community-Collaborations/stempipeline/Teach2Learn/teaching-to-learnUnderthislicense,youarefree:toShare—tocopy,distributeandtransmittheworktoRemix—toadapttheworkandincorporateitintoyourownpracticeUnderthefollowingconditions:Attribution—Youmustattributetheworkinthemannerspecifiedas“TeachtoLearnAttribution”below.Youcannotattributetheworkinanymannerthatsuggeststheprogramorstaffendorsesyouoryouruseofthework.Noncommercial—Youmaynotusethisworkforcommercialpurposes.ShareAlike—Ifyoualter,transform,orbuilduponthiswork,youmaydistributetheresultingworkonlyunderthesameCreativeCommonsAttribution-NonCommercial-ShareAlike3.0license(CCBY-NC-SA3.0).TeachtoLearn’sAttribution:©2016TeachtoLearn.Allrightsreserved.Translations:Ifyoucreatetranslatedversionsofthismaterial(incompliancewiththislicense),pleasenotifyprincipalinvestigator,[email protected]/orlinktosuchtranslatedversions(eitherasis,orasfurthermodifiedbyTeachtoLearn.
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TableofContents
LessonsataGlance Page5UnitPlan Page8LessonFeatureKey Page12EssentialQuestionConceptMap Page13TieredVocabularyList Page16ScienceContentBackground Page18LessonPlans Lesson1:WhatisaPhysicalMap? Page31Lesson2:Mohs’HardnessScale Page39Lesson3:WhatisErosion? Page48Lesson4:WhatisaSoil?IsAllSoiltheSame? Page59Lesson5:FoolingwithFossils Page70Lesson6:EarthquakesandFaultLines Page78Lesson7:ProtectingAgainstNaturalDisasters Page91UnitResources CurriculumEmbeddedPerformance Page1035EInstructionalModelBackground Page107ScienceTalkandOracyinT2L Page108UnitActivityPlanner Page111NGSSAlignmentTable Page117ListofUnitResources Page121
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LessonsataGlance
Independentonlinestudentresearch Technologyintegration YouTubeVideo
Outdooreducation Movement LabworkLesson CoreActivities Extensions AspectsofLesson1.WhatisaPhysicalMap?
• TypesofMaps• TreasureMaps• MapFeaturesReview• LandformReview• WordWarm-Up• PhysicalMapInvestigation• OnlineMaps• DailyPlanetEarthNewspaper
2.Mohs’HardnessScale
• PhysicalPropertiesofMinerals• DescribingMinerals• MohsHardnessScale• MineralObservationStations• MineralIdentification• TheMysteryRockExperiment• MineralAd
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3.WhatisErosion? • WeatheringandErosionPowerPoint
• ErosionandAbrasionStations• WashingAwayLandforms• BerkshireLandforms• Mt.GreylockArticle
• PairedPassages
4.WhatisaSoil?IsAllSoiltheSame?
• SoilExploration• IMOWAChart• SoilDiscovery• SoilRecipe• SoilDrainageTest
• ConnectionstoMountGreylock
5.Fossils • Makeyourownfossil• FossilizationGame• FossilMap• Writeaboutyourfossil
• TriptoBerkshireMuseum
6.EarthquakesandFaultLines
• VolcanoDemonstration• RingofFireActivity• GrahamCrackerPlate
Tectonics
7.ProtectingAgainstNaturalDisasters
• GeoSquadStopsFredtheFloodVideo
• FloodsPowerPoint• “SafeHouses”reading• DisasterPreparednessGame• DinosaurExtinctionDebate• DisasterSurvivalComic
• FloodActivity
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UnitPlan
Stage1DesiredResultsGradeLevelStandards
(4-ESS1-1)Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.[ClarificationStatement:Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.][AssessmentBoundary:Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrockformationsandlayers.Assessmentislimitedtorelativetime.](4-ESS2-1)Makeobservations
MeaningUNDERSTANDINGSStudentswillunderstandthat...
• Physicalmapsshowthelocationsofphysicalfeaturesonland,suchasmountains,rivers,andelevation.
• Local,regional,andglobalpatternsofrockformationsrevealchangesovertimeduetoforcessuchasearthquakes.Thepresenceandlocationofcertainfossiltypesindicatetheorderinwhichrocklayerswereformed.
• Thedevelopment,weathering(howitisbrokendownintosmallerpieces),anderoding(particlesaretransportedelsewhere)oflandformscanhelppeopleinferthehistoryofthecurrentlandscape.
• Rainfallhelpstoshapethelandandimpactthelivingthingsfoundinaregion.
• Liquidandsolidwater,wind,andlivingorganismsbreakrocks,soil,andsedimentsintosmallerparticlesandmovethemaround.
ESSENTIALQUESTIONS 1. Howcanweprotectagainstnatural
disasters?2. Whatcanrockstellusaboutthe
past?3. HowcanmapsmodelEarth’s
features?
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and/ormeasurementstoprovideevidenceoftheeffectsofweatheringortherateoferosionbywater,ice,wind,orvegetation.[ClarificationStatement:Examplesofvariablestotestcouldincludeangleofslopeinthedownhillmovementofwater,amountofvegetation,speedofwind,relativerateofdeposition,cyclesoffreezingandthawingofwater,cyclesofheatingandcooling,andvolumeofwaterflow.][AssessmentBoundary:Assessmentislimitedtoasingleformofweatheringorerosion.](4-ESS2-2)AnalyzeandinterpretdatafrommapstodescribepatternsofEarth’sfeatures.[ClarificationStatement:MapscanincludetopographicmapsofEarth’slandandoceanfloor,aswellasmapsofthelocationsofmountains,continentalboundaries,volcanoes,andearthquakes.](4-ESS3-2)Generateandcomparemultiplesolutionstoreducethe
• Thelocationofmountainranges,deepoceantrenches,oceanfloorstructures,earthquakes,andvolcanoesoccurinpatterns.Mostearthquakesandvolcanoesoccurinbandsthatareoftenalongtheboundariesbetweencontinentsandoceans.
StudentLearningTargets“Ican”statements
1. Icanidentifyaphysicalmapanditscomponents.2. Icanreadmapsthatdepictmountainranges,trenches,activevolcanoes,and
earthquakes.3. Icanperformappropriateteststodeterminethehardness,color,luster,cleavage,and
streakofdifferentminerals.4. Icannotedifferencesbetweenrocksandminerals.5. Icanusepreviouslyrecordeddatatoidentifydifferentminerals.6. Icanobserveanddescribeexamplesofweatheringthroughfrostwedging,abrasion
andtreerootwedging.7. Icanobserveanddescribeexamplesoferosionthroughwind,water,andice.8. Icanexplainthedifferencebetween“weathering”,“erosion”,and“deposition”.9. Icanexplainhowsoilisformedthroughdecompositionandweathering.10. Icanillustratetheconnectionbetweensoilformation(e.g.ratiosoforganicmatterto
minerals)anditscolorandtexture.11. Icanidentifyanddescribethedifferencesbetweensoil,loam,andclay.12. Icanwriteastoryaboutthehistoryofmyfossil.13. Icanexplainthedifferencesbetweentypesoffossils.14. Icanexplainhowplatetectonicscreateearthquakesandmountains.15. Icandiscusshowvolcanoesareformedandtheeffectsoftheireruptionsonland.
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impactsofnaturalEarthprocessesonhumans.*[ClarificationStatement:Examplesofsolutionscouldincludedesigninganearthquakeresistantbuildingandimprovingmonitoringofvolcanicactivity.][AssessmentBoundary:Assessmentislimitedtoearthquakes,floods,tsunamis,andvolcaniceruptions.]
16. Icanmodelhowearthquakes,mountains,andvolcanoesarecreated.17. Icandiscussthreetypesofnaturaldisastersincludingvolcaniceruptions,
earthquakes,andfloods.18. Icandiscusstheimpactsofnaturaldisastersandhowtoprotectagainstorlessenthe
effectsofthesenaturaldisasters.
Stage2–EvidenceEvaluativeCriteria AssessmentEvidenceScienceJournalsClassDiscussionsGrouppresentationsParticipation
PlanetEarthNewspaperJournalentriesClassdiscussionsPracticeMCASquestions
Stage3–LearningPlanLesson1:Inthislesson,studentswillreviewlandforms.Theywillthenbeintroducedtophysicalmaps,bothonlineandonpaper.Lesson2:Studentswilllearnaboutthethreemaincategoriesofrocksandthatrocksaremadefromcombinationsofminerals.TheywillperformMohs’hardnesstesttoidentifyvariousminerals,includingamysterymineral.Lesson3:StudentswilllearnaboutweatheringanderosionthroughaPowerPointandvariousactivities.TheywillanalyzepicturesofBerkshirecountylandformsandtheorizeastohowtheywereformed.
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Lesson4:Studentswilllearnaboutthecomponentsandcharacteristicsofsoil.Then,theywillwriteasoilrecipefortheirnewspaperprojectanddoasoildrainagetestwithdifferenttypesofsoil.Lesson5:Studentswillengageingamesandactivitiestolearnaboutfossils.Theywillmaketheirownfossilsandthenwriteastoryaboutthefossiltheymade.Lesson6:Inthislesson,studentswilllearnaboutvolcanoesandearthquakes.Theywillbuildavolcanoandmodelearthquakesusinggrahamcrackersandcool-whip.TheywillthenmapearthquakesandvolcanoesontheRingofFiretoexploretheconnectionbetweenthetwophenomena.Lesson7:Inthefinallessonoftheunit,studentswilllearnaboutthethingstheyneedtosurvivefromnaturaldisasters,includingonesmentionedpreviouslysuchasvolcaniceruptionsandearthquakes.Thentheywillhaveadebateabouttheextinctionofthedinosaurs.AdaptedfromMassachusettsDepartmentofElementaryandSecondaryEducation’sModelCurriculumUnitTemplate.OriginallybasedonUnderstandingbyDesign2.0©2011GrantWigginsandJayMcTighe.UsedwithPermissionJuly2012
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LessonFeatureKeyLessonsinthisunitincludeseveralfeaturestohelpinstructors.Itisaquickguidetohelpidentifyandunderstandthekeyfeatures.
Icons
Talkscienceicon:Lookforthisicontoletyouknowwhentousesomeofthetalksciencestrategies(foundintheunitresourcesofthisunit)
Anchorphenomenonicon:Indicatesatimewhenananchoringscientificphenomenonisintroducedorwhenanactivityconnectsbacktothisimportantidea.TextFormatting:[SP#:….]Anytimeyouseeasetofbracketslikethis,itindicatesthatstudentsshouldbeengagedinaspecificscienceorengineeringpractice.Underlinedtextinthelesson:Thisformattingindicatesimportantconnectionsbacktothecentralscientificconceptsandisusefultonotetheseconnectionsasaninstructor,aswellasforstudents.
CalloutsTeachingTip
Inthesecall-outboxes,you’llfindtipsforteachingstrategiesorbackgroundinformationonthetopic.
StudentThinkingAlertLookoutforcommonstudentanswers,waysinwhichstudentsmaythinkaboutaphenomenon,ortypicalmisconceptions.
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EssentialQuestionConceptMaps
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TieredVocabularyListTier1 Tier2 Tier3
Color
Soil
Clay
Loam
Sand
Continents
Hardness
Streak
Texture
Decomposition
Decaying
Landforms
Particles
Scale
Boundaries
Prehistoric
Earthquake
Fossil
Sedimentary
Igneous
Metamorphic
Mineral
Crystal
Luster
Cleavage
Frostwedging
Treerootwedging
Weathering
Trenches
CompassRose
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Erosion
Flood
Redirect
Contain
Withstand
Barrier
FaultLines
TectonicPlates
Organic
Inorganic
Jurassic
Abrasion
Legend
Prevention
Extinction
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ScienceContentBackground
Pleasereadthroughtheexplanationprovidedinthenextfewpagesandjotdownquestionsoruncertainties.Consultinternetresourcestoansweryourquestions,askcolleagues,andworktogetherasateamtogrowyourownunderstandingofthesciencecontentandthecentralphenomenainthisunit.Thisknowledgeprimesyoutobetterlistenandrespondtostudentideasinproductiveways.Pleasefeelfreetorevisitthisexplanationthroughouttheunittoreviseandimproveyourownunderstandingofthesciencecontent.
EssentialQuestions
1. Whatcanrockstellusaboutthepast?Rocksareanessentialgatewayintothepastforscientists.Theycontaininformationsuchasthedatesoftherockandthetypesoforganismsthatmaybelivingaroundorinsideofthem(preservedasfossils).TheEarth’scrustlayerscantellusaboutthedifferenttimeperiodsthatorganismslivedinandthetypesofactivitythatoccurred.
2. Howcanweprotectagainstnaturaldisasters?Therearemanywaysthatlivingorganismshelpprotectagainstnaturaldisasters.First,wemustdeterminehownaturaldisastersoccurtoconstructplansforprotectinglivingorganisms.Therearemanyprotectionmethodsagainstdisasterssuchasbarriers,falloutplans,andshelters.However,theprotectionmethodyouimplementdependsonthetypeofdisaster.
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3. HowcanmapsmodelEarth’sfeatures?
Therearemanytypesofmapssuchastopographicmaps,physicalmaps,politicalmaps,etc.EachtypeofmapfocusesondifferentaspectsoftheEarth’ssurfacetomodeldifferentfeatures.Inthisunit,studentswillprimarilyusephysicalmapswhichshowthephysicalfeaturesoftheEarth.StudentswilllearntoidentifyEarth’sfeaturesonthemapandhowfeaturescanberepresentedinseveraldifferentways.Inaddition,studentswilllearnthatsincemapsarerepresentationsoftheworld,theyarenotabletorepresenteverything.Forthisreason,mapmakersutilizesymbolstoindicateEarth’sfeatures.
RationaleforOrderofContentSincethisunitfocusesontheEarth’ssurface,webeginthisunitwithareviewofthemappingaspectsfoundinthesecond-gradeunit,LandandWater.Similartothesecond-gradeunit,mappingwillserveasatooltohelpstudentslearnabouttheEarth’sfeatures.Fromavarietyofmapssuchastopographicalmaps,studentswillseehowEarth’ssurfaceiscomposedofmanycomponentssuchaslandforms.OncethestudentsgainanunderstandingoftheEarth’ssurfacefeatures,studentswilllearnaboutthefundamentalbuildingblocksoftheEarth’ssurface,mineralsandrocks.TheGeoSquad,agroupofanimatedrocks,willguidestudentsthroughMohs’HardnessScaleandthestudyofrocksandminerals.Bylearningabouttheformationofdifferenttypesofrocks,studentswilllearnhowlandformstheysawinthefirstlesson,WhatisaPhysicalMap?,werecreated.Furthermore,withthisknowledge,specificallyaboutsedimentaryrocks,studentswilldeveloptheirunderstandingthattheplanet’ssurfaceisshapedovertimebynaturalforces.Then,inthethirdlesson,WhatisErosion?,studentswilllearnabouterosionastheydiscoverthewaysrocksandmineralsarebrokendown.Thislessonwillexpanduponstudents’understandingofhownaturalforcessuchasweatheringshapeEarth’ssurface.Besidesthis,erosionwillteachstudentsthatrocksvarywithage,sostudentscancorrectanymisconceptionthatrocksareallthesameage.
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Inthisway,studentswilllearnthattheEarth’scrustiscomposedofmultiplelayersandthetopmostlayersarenewerincomparisontothebottomlayers.Thisidea,alongwiththeprocessofcreatingEarth’slayers,willbecoveredinlessonfour.Inthislesson,studentswillapplyknowledgeoferosiontolearnhowrocksandmineralsarebrokendowntocreatesoil.Inthesecondhalfofthisunit,theanchoringphenomenoninvolvingfossilsanddinosaurs,willbemoreobvioustostudents.Inthefifthlesson,studentswilllearnaboutfossilsinmoredepth.Sincestudentslearnedaboutsoilcomponentsinthefourthlesson,theywillusethisknowledgetolearnhowsometimesthedecayingorganicmatterinsoiliscompressedunderlayersofsoil,turningthemintostoneorfossils.Thislessonwillalsoconnectbacktothedinosauranchoringphenomenonbecausedinosaurfossilswerealsocreatedinthisway.Fromthislesson,studentswillunderstandwhyarchaeologistsmustdigdeeptofinddinosaurfossils,sinceittakesyearsoferosiontocreatethelayersofsoiltoburythedinosaurcarcassesandturnthemintostone.Next,studentswilllearnabouttheouterlayeroftheEarth’ssurface,thecrust,inthesixthlesson.Specifically,studentswillbetaughtthatthecrustiscomposedoftectonicplatesthatareconstantlymoving.Duetothemovementoftectonicplates,naturaldisasterssuchasearthquakesandvolcaniceruptionsoccur.Basedonthisinformationabouttectonicplates,studentswillbeabletoconcludethattheplatemovementsthatcreatevolcanoescouldhavecausedthedinosaurs’extinction.Inadditiontonaturaldisasters,studentswillusetheirknowledgeofmetamorphicrockformationtolearnhowlandformssuchasmountainswereformedinthislesson.Finally,studentswillcoverseveralwaystolessentheeffectsofnaturaldisasters.Inthelastlesson,studentswilllearnthatsolutionsfornaturaldisastersvarydependingonthetypeofnaturaldisaster.Forinstance,floodchutescancontainfloodwaters,buttheycannotcontainthedamagecausedbyearthquakes.
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AnchoringPhenomenonThelessonsinthisunit,especiallythelastthree,aretiedtogetherbythestoryofdinosaursandthemysteryoftheirextinction.Inlessons3and5,thestudentslearnabouthowdinosaurs’remainsformfossils.Inlesson6,thestudentsareintroducedtodisasterssuchasvolcanoesandearthquakesandthedisasters’possibleroleinwipingoutthedinosaurs.Inlesson7,theywillbepresentedwithevidenceofthedinosaurs’extinctionandhavetheopportunitytodebatepossibletheories.Therearestillsomemysteriessurroundingtheextinctionofthedinosaurs,butforthisunit,wechosethemostwidelyagreed-ontheoryastheanswertotheanchoringphenomenon.WeknowthatneartheendoftheMesozoicperiod,volcanoesintheDeccanTrapsstartedexploding.Consequently,theairwasfilledwithashandgreenhousegases.Then,manydinosaursbegantogoextinct,causingthenumberofdinosaurspeciestodecline.Aquartermillionyearslater,a6-milewideasteroidslammedintotheYucatanpeninsula,formingtheChicxulubCrater.Itcreated300-foot-widetsunamiwavesand10.0-magnitudeearthquakesacrosstheGulfofMexico,coveringtheareainrocks.Theexplosioncreatedanenormouscloudofdustthatenvelopedtheearth.Thedustthencooledintopiecesofburningglassthatraineddownfromtheskyandheateduptheatmosphere,causingforeststoburstintoflame.TheripplestheasteroidsentthroughtheEarthmayhaveevenpushedmagmatothesurfaceandcausedvolcanoestoexplodeevenfasterforthenext500,000years.ThesmokefromtheDeccanvolcanoes,theasteroid,andtheburningforestsblackenedtheworld’sskiesforyears,throwingtheplanetintotwilight.WithouttheSun’sraysshiningontheearth,plantsdiedoffandtheworld’stemperaturedroppeddramatically.Bythetimetheashclearedup,theatmospherewasfilledwithgreenhousegases,causingtheEarthtoexperiencedramaticclimatechangeduetoglobalwarming.Allthesenaturaldisastersweremorethanenoughtokillofflargeanimalsonlandandsea,butsmallanimalslikebirds,reptiles,andmammalsmanagedtosurvive.
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KeyScienceIdeas• Mappinghas4components:title,key,compassrose,scale.• Thereareavarietyofmapssuchastopographicalmaps,physicalmaps,etc.• Thephysicalpropertiesofmineralsincludehardness,color,luster,cleavage,andstreak.• Rockscanbecomposedofoneormanyminerals.• Mohs’HardnessScalecanbeusedtoidentifydifferentminerals.• SoilistheupperlayeroftheEarth’ssurfaceandithasfivecomponents:Inorganicmatter,Microorganisms,Organic
matter,WaterandAir(IMOWA).• Someinorganicmattercomesfromnaturalprocessessuchasweathering,andotherssuchascoinsandbottlescome
frompollutioncreatedbyhumans.• Microorganismsaresmalllivingbeingsthatliveinthesoil.• Organicmatterrepresentslivingbeings,deadanimals,andplantsandmattercomingfromlivingorganisms.• Waterandairarefoundinthespacebetweensoilparticles.• Decompositionisabiologicalandphysicalbreakdownoforganicmattersuchasleaves,deadanimals,andplantsinto
simplerorganicmatter.• Soilisformedthroughtheprocessoferosionandweathering.• Erosionisageologicalprocessthroughwhichrocksarewornawayandcarriedtoanotherlocationbynaturalforces
suchaswindandwater.• Weatheringisaprocessbywhichrocksbreakdownintosmallerpieces.• Therearethreetypesofweathering:physicalweathering,biologicalweathering,andchemicalweathering.• Allsoilsarenotthesamebecausetheyhavedifferentcolors,texture,andwaterretentioncapacities.• Therearethreedifferentformsoffossilsinthisunit:bodyfossils,tracefossils,andmoldfossils.
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• Fossilsarefoundinsedimentaryrock.Thisisbecausesedimentaryrockisthesoftestformofrock;itallowsthefossiltositintherockandhardenovermanyyearswithoutbeingcrushedbytheweight.
• Erosionisamajorreasonthatfossilscanformandthatweareabletodiscoverthem.Waterisfundamentaltofossilsforming,asitseepsintothefossilandhelpsturnittostoneovermillionsofyears.
• TheoutermostlayeroftheEarthiscalledthecrust,andthecrustisbrokenintopiecescalledtectonicplates.• Earthquakesoccurwhentwotectonicplatescollideorslideagainsteachother,andenergyisreleased.• Whentwoplatescollideandthelandshiftsupward,mountainsarecreated.• Whenplatescollide,andapieceofanoceanicplatebreaksoff,magmarisestothesurfaceandhardens,creatinga
volcano.
ExplanationMineralsandRocks
• Amineralisaninorganicsolidwithadefinitechemicalcompositionandacrystallinestructureformedbygeologicalandnaturallyoccurringprocesses.Arockisacombinationofoneormoreminerals.Theymayalsoincludeorganicremainsandmineraloidswhileothersarepredominantlycomposedofjustonemineral.Therearethreetypesofrocks:igneous,metamorphic, and sedimentary. Sedimentary rocks are formed from particles called sediment,which includes sand,shells, pebbles, andother fragmentsofmaterial.The sediment accumulates in layers andover a longperiodof timehardensintorock.Sedimentaryrockistypicallysoftandmaybreakapart/crumbleeasily.Sedimentaryrocksareusuallytheonlytypethatcontainsfossils.MetamorphicrocksareformedunderthesurfaceoftheEarthfromthechangethatoccursduetointenseheatandpressure.Igneousrocksareformedwhenmagmacoolsandhardens.
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TheMohsHardnessScale• TheMohsHardness Test is used to identify amineral type. This test compares the resistance of amineral to being
scratchedbytenreferencemineralsknownastheMohsHardnessScale.Thetestisusefulbecausemostspecimensofagivenmineralareveryclosetothesamehardness,whichmakeshardnessareliablediagnosticproperty.Thescalegoesfrom1-10,with1beingthesoftestmineral.Thescale isas follows:Talc,gypsum,calcite, fluorite,apatite,orthoclase,quartz,topaz,corundum,diamond.
Soil,ErosionandWeathering
• SoilFormation:Soilisformedthroughtheprocessoferosionandweathering.Erosionisageologicalprocessthroughwhichrocksarewornawayandcarriedtoanotherlocationbynaturalforcessuchaswindandwater.Erosioncanalsocarry soil and sediments. Weathering is a geological process bywhich rocks break down into smaller pieces. Thedifferencebetweenweatheringanderosion is thaterosion involvesdisplacement. Thereare threedifferent typesofweathering:➢ PhysicalorMechanicalweatheringisduetophysicalforcesactingonrocks.Sometimesrainwaterwillsoak
intorockandthenfreeze,expandingasitdoes.Withenoughcyclesoffreezingandmelting,thewaterwillcreatelargecracksintherockandcausepiecestobreakoff.Italsooccurswhenmovingwaterrubsrocksagainsteachother, also causing tiny pieces to break off. The rubbing the rocks experience is very gentle and slow-paced,however,sotheyoftenlookmorelikethey’vebeensandeddownthanbrokenapart.
➢ Biological weathering is due to the presence of living organisms such as plants, bacteria and animals. Forexample,treesarealwayssendingoutrootstofindnutrientsandincreasetheirholdontheground;sometimesthoserootscanevenpassoverbarerock.Iftherootsdoendupfindingsoilafterstretchingoverarock,theywillgrowthickerandthicker,eventuallysqueezingtherocklikeaboaconstrictor.Underthatpressuretherockwill
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crack.➢ Chemicalweatheringisduetochemicalprocessessuchasoxidationandacidification.Forexample,watercan
dissolvecertaintypesofsoftrock.Incaves,waterwilldripfromtheceiling,bringingwithitpiecesofdissolvedrock.Overtimetheseresidualpiecesofrockaddupandformstalactitesontheceilingandstalagmitesonthefloor.
• Erosionismainlyduetowindandwater.Inliquidform,watercancarryawaypiecesofrockwhilemovinginariver,flood,orwave.Insolidform,watermovesdirtandrockasaglacier.Glaciersarelargesheetsoficethatflowdownmountainsidesinthesamemannerasrivers,onlymuchmoreslowly.Glaciersareoftenagreatdeallargerthanrivers,andasaresulttheycancarveouthugepiecesofrockandlargequantitiesofgravelfromthemountainstheyrollover.Consequently,intheprocess,glaciersdecreasethemountains’heightandcarveoutlargevalleys.Berkshirevalleyisoneofthegreatestexamplesofglacialerosion.Theentirevalleywascarvedbyglaciers.BalanceRockintheBerkshiresisapieceofamountainthatwasleftbehindbyameltedglacier.
• Windoftenplaysanimportantroleinthelandscapesofdryareas.Windscarrylargequantitiesofsandanddustforthousandsofkilometers.Sometimesthewindscanblowawayfertilesoil,makingtheareadrierandhardertofarm.Thesandsthatwindscarrycanblastagainstrocksastheytravelintheair,scarringtheirsurfaceswithlinesandwearingthemaway.
• Soilisformedwhenrocksbreakdownthroughtheprocessofweatheringandthesmallerrockpiecesarecarriedawaybyair,wind,andgravityandaccumulateinaregion.Also,whenrocksbreakdown,theyreleasemineralswhichmakethesoilrich.Then,thesoilaccumulatesairandwaterwhichthenleadstothedevelopmentofmicroorganisms,plantsandanimals.Whensomeofthelivingbeingsdie,theyaredecomposedandturnedintosimplerorganicmatterthatenrichesthesoil.Tonote:thisprocessofsoilformationtakesaverylongtimetooccur.
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ComponentsofSoil• Soil is theupper layerof theEarth’ssurface,madeupof fivedifferentelements: Inorganic,Microorganisms,Organic,
WaterandAir(IMOWA).Generally,“ideal”soilismadeupof45%inorganicmatter,25%air,25%waterand5%oforganicmatterandmicroorganisms.
• Inorganicmatter is a soil element that does not come from any livingmatter. This is usually the product of rockweatheringandoftenreferredtoasdirt.Someinorganicmaterialsincludesand,clay,siltandloam.Sandparticleshaveadiametersizebetween0.05to2mm,clayhasparticleswhosediametersizeisbetween0.002and0.05mmandfinallysiltparticleshaveadiametersizelessthan0.002mm.Loamisamixtureofsand,clayandsilt.Usually,loamcontainsanequal proportion of sand and silt and a small quantity of clay. Additionally, there are someother types of inorganicmaterialsthatdonotoriginatefromnaturalprocesses.Thesematerialsincludecoins,bottles,plasticbags.Theyfindtheirwayintothesoilduetopollutionbyhumans,whichultimatelycanharmthesoil.
• Microorganismsareextremelysmalllivingorganismsthatcanbeveryhardtoseewiththenakedeye.Soilistheirhabitatand some of the microorganisms contribute to the process of decomposition, which is a biological and physicalbreakdownoforganicmattersuchasleaves,deadanimalsandplantsintosimplerorganicmatter.
• Organicmatterismadeupofelementsthatarelivingorganismsorcomefromlivingorganisms.Organicmatterincludesplants,deadanimalsatvariousstagesofdecompositions,andmicroorganisms.
• WaterandAiraretheremainingcomponentsofsoilandtheyarenecessaryforthesurvivaloflivingorganisms.Theyarefoundinthespacebetweensoilparticles.
• Allsoilsarenot thesameandthesedifferencescanbeexplainedbythesoilcomposition.Wecanseethedifferencesbetweensoilsbylookingattheirtexture,colorandwaterretentioncapacity.
• TextureandWaterretentioncapacity:Soiltexturedependsonthesizeoftheparticlesthatmakeupthesoil.Thesizeoftheparticlesalsoaffectstheabilityofthesoiltoretainwater.Forinstance,sincesandhaslargeparticlesthatcannotbepackedtogetherperfectly,watermovesveryeasilybetweenthegaps.Clayhasvery fineparticlespackedtogether
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whichmakesithardforwatertomove,henceclayretainswaterverywell.• Color:Thecolorofthesoildependsontheproportionofitsfiveconstituents.Forinstance,ablack-coloredsoilindicates
ahighcontentinorganicmatterwhereasayelloworredsoilindicatesahighcontentinironoroxidizedmaterials.• Soilisimportantbecauseitisahabitatforseveralanimals,plantsandmicroorganisms,astorageofnutrientsforliving
beings,andananchorforplants.Fossils
• Fossilstakemillionsofyearstoform.Thereareafewfactorsthatmustbepresenttomakeafossil.First,theorganismmustbeburiedquicklyafterdeath.Someofthemostcommonplacestofindfossilsareriverbedsoroceanfloorsbecausethemovementofthewaterhelpsburytheorganisminthebottomofitsdepthswherethefossilizationprocesscanbegin;fossilsarelargelyfoundinsedimentaryrock.OnceundergroundthefossiltakesinwaterandmineralsfromtheEarth,slowlyreplacingthetissueoftheorganismwithminerals.Again,thistakesaverylongtimetohappen.Compressionfromtheweightofthegroundabovehelpsthisprocess.Erosionisalargepartofwhyfossilsexistaswellaswhytheyarefound.Ifitweren’tforerosion,fossilswouldn’thavebeenburiedtobecomewhattheyare,andtheywouldn’thavebeenunburiedtobediscoveredbyhumanbeings.
• Therearediversetypesofexistingfossilsintheworld.Forthisunitwewillspecificallyfocusingonthreemainversions:body fossils, trace fossils, andmold fossils. These are the types of fossils archeologistsworkwith themost in theirprofession.➢ Bodyfossilsaretheremainsofadeadanimalorplantandarethemostcommonfoundfossilsintheworld.These
aredinosaurbones,petrifiedtrunks,shells,etc.Duringtheprocessoffossilizationhardtissuesuchasboneandbarkarefarmorelikelytobecomefossilsbecauseofthenatureoftheirmakeup.Softtissuetendstowearaway;whetherthatbefromerosion,water,wind,orotherorganismssuchasfungioralgaethateatthem.Organismsthatdonotwearawaymustthenbeburiedinsediment.Crustaceansandshellsthatliveontheoceanfloorare
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muchmorereadilyfossilizedbecausetheyarealreadyinasediment.➢ Tracefossilsarestructurespreservedinsedimentthatrepresentstheorganism’sbiologicalanatomy.Theseare
thingslikefootprintsorburrows.Aseashellrollingalongtheoceanfloorisnotanexampleofatracefossilbecauseittellsnothingoftheorganism’sanatomy.Thebodilystructureandfunctionoftheanimalisthekeyaspectofatracefossil.Theyareveryseldomfoundwithabodyfossil,andtheyarehardtomatchbacktoananimal,thereforetheyareclassifiedbytheactivitytheyareperformingratherthantheanimaltheyreferto.
➢ Moldfossilsareexactlywhattheysoundlike,amoldofanorganism.Thismeansthatalifeformhadbeenlyinginthesediment longenoughforthesurroundingrocktoharden, leavingan impressionof theorganism,andtheorganismwearsaway,leavingonlythemoldofitsbody.Examplesincludeimpressionsofshellsorleavesimprintedonarock.
• Hereisalinktomoreinformationabouttheseaswellasothertypesoffossils:http://www.fossilmuseum.net/fossilrecord/fossilization/fossilization.htmEarthquakes,Faultlines,andVolcanoes
• Tobegin,teachersmustunderstandthattheEarthismadeofmanylayers,theoutermost layerofwhichiscalledthecrust.Thecrustisbrokenupintopiecesthatarecalledtectonicplates.Thislessoncoverstwotypesofboundariesthatoccurwhentectonicplatesinteractwitheachother.Theseboundariesarecalledtransformboundariesandconvergentboundaries.Atransformboundaryoccurswhentwotectonicplatesrubtogether.Asthepressurebuildsbetweentheplates, theyslipreleasing theenergy thatweperceiveasanearthquake.Aconvergentboundaryoccurswhentwotectonicplatescollidewitheachother.Asthetwoplatescollidetheyformmountainsbetweenthemasthelandshiftsupward.Thislessonalsocoversthecreationofvolcanoeswhichoccursatasubductionzone.Asubductionzoneoccurswhenadenseroceanicplateisthrustunderneathalessdensecontinentalplate.Apieceoftheoceanicplatebreaksoffandmeltsallowingformagmatocometothesurface.Thismagmahardensandformswhatweknowasavolcano.
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ProtectingAgainstDisasters
• NaturaldisastersareanyEarthprocessesthatharmanddestroylivingcreaturesandthethingstheyneedtosurvive.Naturaldisasterscanhappenveryslowly,suchasmajordroughts,orveryquickly,suchasearthquakes.Thepriorityindealingwithnaturaldisastersistofindoutwhetherwecanpreventthemfromhappening.
• Thekeytopreventingdisastersistofigureoutwhatmakesthemhappen.Forexample,floodsoccurwhenthereismorewaterinanareathanthegroundcanabsorb.Wecansometimespreventthegroundfrombeingoverloadedwithwaterbygrowingplantsorsettingupraincatchersorfloodchutes.
• Humanscan’tpreventeveryfloodfromhappening,andtherearesometypesofnaturaldisasterswecan’tpreventatall.Somedisasterslike,earthquakes,andvolcaniceruptionswillhappennomatterwhathumansdo.That’swhyit’susefultobeabletofigureoutwhennaturaldisastersaremostliketohappen,sothatwecanstartmovingpeopleandvaluableobjectsoutofharm’swaywhilewestillhaveenoughtime.Ofcourse,noonecanfullypredictnaturaldisasters;justlikeaweatherforecast,thebestwecandoisfigureoutwhenthereisagoodchancethatanaturaldisasterwillhappen.
• Meteorologistscanoftentimesforecastblizzards,hurricanesandtornadoesandfigureoutthepathstheyaregoingtotakeoncetheyform.Volcanologists,whostudyvolcanoes,alsohavetoolsattheirdisposal.EruptionsoftenstartwhenmagmaisreleasedfromdeepwithintheEarthbyshiftingplates.Theseplatesalsosetoffsmallearthquakes.Bylisteningcarefullytotheseearthquakes,volcanologistssometimesrealizethatitsoundslikeenoughmagmahasrisentotriggeraneruption.Thebubblingmagmaalsoreleasesgasessuchascarbondioxideandsulfurdioxidethataredifferentfromthegasesthatthevolcanoreleaseswhenitisn’tgoingtoerupt.Bymeasuringthesegases,volcanologistscantellwhenavolcano’smagmaisrising.Lastly,asvolcanoesfillupwithgasandmagmatheyoftenstarttobulgeabitlikeaninflatingballoon.Byplacingsensorsonthevolcano,volcanologistscanmeasurethisbulge.
• VolcanologistssawwarningsignsliketheseonMt.PinatuboandMt.St.Helensweeksbeforetheyerupted,andboth
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timeswarnedpeopleinthesurroundingareastoevacuate.Someestimatethattheseevacuationssavedtensofthousandsoflives.
• Byfar,earthquakesaretheworstunderstoodandthehardesttopredictofEarth-basednaturaldisasters.Thebestwecandoislookatthehistoryofcertainfaultlinestoseeiftheearthquakesinthatareafollowapattern.Seismologists(earthquakescientists)arealsoabletocalculateifafaultis“woundup”enoughtotriggerabigearthquake,butthatonlytellsusthatanearthquakecouldhappen,notthatitwillhappen.
• Lastly,therearecaseswherewecan’tpreventorpredictnaturaldisastersormightnotbeabletomoveeveryoneandeverythingtosafety.Inthatcase,wecaneitherredirectthedisaster,containit,orwithstandit.
• ThefloodchutesinNorthAdamsredirectfloodwatersintheHoosicRiverfromspillingontothestreetsinthetown.Redirectinglavaflowsiscomplicatedanddangerous,butithasbeendone,especiallyonslow-movinglava.In1982,peopleredirectedthelavacomingoutofMt.Etna,inSicily,bybuildinghugeEarthwallswithbulldozersasthelavacamein.Theyevencarvedoutchannelsfromthethicker(butstillveryhot!)lavaanddeepenedthembysettingoffexplosivesinsidethem.
• Reservoirscancontainfloodwatersbytrappingthem,sotheydon’tgettosensitiveareas.ThecityofHoustonhaslarge,low-lyingareasfilledwithtreesandgrassthataredrymostofthetime,butfillupwithwaterduringfloods.In1971inIceland,peoplewereevenabletocontainlavabyconstantlysprayingitwithcoldseawater.Thelavahardenedintoathickwallthatkeptthenewer,moltenlavabehinditfromcominganycloser.
• Lastly,wecanbuildthestructureswewanttoprotectsothattheycanwithstanddisasters.Dikesandseawallswithstandstormsandfloodsandprotecteverythingbehindthem.Peoplewholiveinearthquake-proneareascanfirmlyattachheavyobjectsoffurnitureintheirhomestothewallsandground,sotheywon’ttipover;theycanalsoreinforcethewallsoftheirhouseswithplasticmesh,bamboo,andshatter-proofglasswindowssotheyarehardertobreak.
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Sometimesthebestwaytowithstandanearthquakeisnottostaystillbuttogowiththeflow;themostmodernearthquake-resistantskyscrapersarebuiltonspringsandballbearingssothattheyswaywithanearthquake,insteadofgettingtornapartbytheshaking.
Mapping
• Inthislesson,studentswillreviewmapfeaturesandhowtoreadamap.Inthelaterlessonsofthisunit,mapswillbeusedtocommunicateinformationabouttheplacementof fossilsontheEarth’ssurface. Inaddition,studentswillusemapsas tools to learnhow theplacementof tectonicplates canpredictnaturaldisasters, suchas in the ringof fire.Therefore,tolearnaboutnaturaldisastersandfossils,studentsmustfirstlearnaboutmapreading.Althoughmappingisnot integraltothesciencetaught inthis lesson, it isatoolandmodelusedfor learning.Thus,teachersneedtoteachmappingasanothermethodforlearning.
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Lesson1:WhatisaPhysicalMap?
LESSONBACKGROUND
Inthislesson,studentswillreviewmapfeaturesandhowtoreadamap.Inthelaterlessons,mapswillbeusedtocommunicateinformationabouttheplacementoffossilsontheEarth’ssurface.Inaddition,studentswillusemapsastoolstolearnabouttheplacementoftectonicplatesandhowthatcancausenaturaldisasters.Tolearnaboutnaturaldisastersandfossils,studentsmustfirstlearnaboutmapreading.Althoughmappingisnotintegraltothesciencetaughtinthislesson,itisatoolandmodelusedforlearning.Thus,teachersneedtoteachmappingasanothermethodforlearning.ScienceContentBackgroundSincemapsareessentialinthisunit,teachersshouldunderstandthedifferenttypesofmaps.Specifically,physicalmapsandtopographicmaps.Unlikepoliticalmapswhichdepictstateboundaries,physicalmapsdepictlandformssuchasmountainsanddeserts.Similarly,topographicmapsshowlandformsandoceanbodies.However,unlikephysicalmapswhichshowlandformsasflat,topographicmapsuserelieftoshowtheelevationsoftheland.Forinstance,mountainrangesontopographicmapsareshownwithconcentriclinesthatshowtheelevationgain.Furthermore,teachersshouldunderstandthatsincemapsarerepresentationsoftheland,theyonlyfocusoncertainaspectsoftheland.Tohelpmakereadingamapeasier,symbolsarealsoused.Forthisreason,teachersneedtokeepinmindthatmapsdonotshoweverythinginanarea.OverviewoftheLessonStudentswillreviewmapfeaturesandlandformsbylookingatavarietyofmapsanddoingatreasurehunt.Then,theywillinvestigatedistincttypesofmapstonotesimilaritiesanddifferencesbetweenthemaps.StudentswillalsouseGoogleEarthto
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exploreonlinemappingoptions.Finally,fortheirDailyPlanetEarthNewspaper,studentswillcreateaphysicalmapofMassachusetts.FocusandSpiralStandard(s)FocusStandard:4-ESS2-2.AnalyzeandinterpretmapsofEarth’smountainranges,deepoceantrenches,volcanoes,andearthquakeepicenterstodescribepatternsofthesefeaturesandtheirlocationsrelativetoboundariesbetweencontinentsandoceans.SpiralStandard:2-ESS2-2.Maptheshapesandtypesoflandformsandbodiesofwaterinanarea.ClarificationStatements:
• Examplesoftypesoflandformscanincludehills,valleys,riverbanks,anddunes.• Examplesofwaterbodiescanincludestreams,ponds,bays,andrivers.• Quantitativescalinginmodelsorcontourmappingisnotexpected.
SpiralStandard:6.MS-ESS2-3.Analyzeandinterpretmapsshowingthedistributionoffossilsandrocks,continentalshapes,andseafloorstructurestoprovideevidencethatEarth’splateshavemovedgreatdistances,collided,andspreadapart.ClarificationStatement:
• Mapsmayshowsimilaritiesofrockandfossiltypesondifferentcontinents,theshapesofthecontinents(includingcontinentalshelves),andthelocationsofoceanstructures(suchasridges,fracturezones,andtrenches),similartoWegener’svisuals.
StateAssessmentBoundary:• Mechanismsforplatemotionorpaleomagneticanomaliesinoceanicandcontinentalcrustarenotexpectedinstate
assessment.
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SpiralStandard:7.MS-ESS2-2.ConstructanexplanationbasedonevidenceforhowEarth’ssurfacehaschangedoverscalesthatrangefromlocaltoglobalsize.ClarificationStatements:
• Examplesofprocessesoccurringoverlargespatialscalesincludeplatemotion,formationofmountainsandoceanbasins,andiceages.
• Examplesofchangesoccurringoversmall,localspatialscalesincludeearthquakesandseasoningweatheringanderosion.
SpiralStandard:8.MS-ESS2-1.UseamodeltoillustratethatenergyfromEarth’sinteriordrivesconvectionsthatcyclesEarth’scrust,leadingtomelting,crystallization,weathering,anddeformationoflargerockformations,includinggenerationofoceanseaflooratridges,submergenceofoceanseafloorattrenches,mountainbuilding,andactivevolcanicchains.ClarificationStatement:
• Theemphasisisonlarge-scalecyclingresultingfromplatetectonics.W.4.9Drawevidencefromliteraryorinformationaltextstosupportanalysis,reflection,andresearch.NGSSAlignmentScience/EngineeringPractice(SP) DisciplinaryCoreIdea(DCI) CrossCuttingConcepts(CCC)SP2:DevelopingandusingmodelsSP4:Analyzingandinterpretingdata
ESS2.B:PlateTectonicsandLarge-ScaleSystemInteractionsThelocationsofmountainranges,deepoceantrenches,oceanfloorstructures,earthquakes,and
Patterns:Patternscanbeusedasevidencetosupportanexplanation.(4-ESS2-2)
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volcanoesoccurinpatterns.Mostearthquakesandvolcanoesoccurinbandsthatareoftenalongtheboundariesbetweencontinentsorneartheiredges.MapscanhelplocatethedifferentlandandwaterfeaturesareasofEarth.(4-ESS2-2)
LearningTargetsIcanidentifyaphysicalmapanditscomponents.Icanreadmapsthatdepictmountainranges,trenches,activevolcanoes,andearthquakes.AssessmentStudentswillcreateaphysicalmapofMassachusettsfortheirDailyPlanetEarthNewspaper.
WIDALanguageObjectives(DependentontheneedsofyourELLstudents)TargetedAcademicLanguage/KeyVocabularyTier1:ContinentsTier2:Scale,BoundariesTier3:Legend,Trenches,Compassrose
RESOURCESANDMATERIALS
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Quantity Item Source
1map Politicalmap Bin
1map Roadmap Bin
1map Attractionmap Bin
1map Topographicalmap Bin
1map Physicalmap Bin
1map Weathermap Bin
1perstudent Laptop/iPad ClassroomTeacher
1perstudent MapFeaturesWorksheet CMCWebsite
1perstudent GoogleEarthWorksheet CMCWebsite
1perstudent BlankTemplateofMassachusetts CMCWebsite
**Itemsinboldshouldbereturnedforusenextyear**
LESSONDETAILS
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LessonOpening/Activator
1. TypesofMaps:Beforethestudentscomeintotheclassroom,displaythedifferenttypesofmapsavailableontablesaroundtheclassroom.Then,askthestudentstogoaroundtheroomtonotethesimilaritiesanddifferencesbetweenmaps.Next,havethestudentsreturntotheirseatsforaclassdiscussion.Theyshouldrecognizethatnotallmapsarethesame.Differentmapsareneededtorepresentdifferentthings.Askthestudentstodeterminewhatisuniqueabouteachmapandwhatmakessomeofthemapssimilar.Theteachershouldwritethesesimilaritiesanddifferencesontheboard.Also,askthestudentstolookforpatternsonthemaps.(SP4:Analyzingandinterpretingdata)
2. TreasureHunt:Theteachersshouldbesuretohidethe“treasure”beforethestartofthisactivity.Theteachercan
decidewhattohideas“treasure”.Thentakethestudentsoutsideandsplitthemupintogroupsofthreeorfour.Thenumberofstudentsinyourclasswilldeterminethenumberoftreasuresyoumusthide.Teachersshouldsearchcreateasimplemapoftheplayground/outdoorareathestudentswillbeexploringforthisactivity.Thestudentswillthenbegivenmapsandtoldthatthereistreasureontheplaygroundthattheymustfindusingthemap.Givethem10-15minutestotryandachievethistask.Askthestudentstocounttheirpacesastheygofromlocationtolocationontheplayground,withsomeonerecordingthenumbersastheygo;thiswillgivestudentsagraspofscalewhenitisdiscussed.Thisisagreatformativeassessmenttoseeifthestudentsrememberhowtoreadamapfromtheirsecond-grademappingskills.Iftheteacherdeemsitnecessary,assignrolestostudentsfortheactivity:havesomeonedirectthegroupbasedonthemap,someonecanbethediggerforthetreasure,someonecancountoutpaces,etc.Theteacherorsciencefellowmayhelpifthestudentsarehavingdifficultyreadingthemap.(SP2:Developingandusingmodels)
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DuringtheLesson
1. MapFeaturesReview:Studentswillreviewthefeaturesofamapusingthe“mapfeatures”worksheet.Thefeaturesarekey,title,scale,andcompass.Eachpicturecontainsamapfeaturehighlightedinaredbox.Studentsneedtomatchthehighlightedfeaturewiththeappropriateword.Tonote:studentsdidnotlearnaboutscaleinsecondgrade.Therefore,theteacherorsciencefellowshouldusethetreasurehunttoexplaintheconceptofscale.
2. Now,askthestudentshowtheymeasuredthedistancesbetweenlocationsontheirtreasuremaps.Theanswershouldbethenumberofpacestheytook.Tellthestudentsthatthenumberofpacestheyrecordedonthetreasurehuntisthescaleusedonthetreasuremap.Scaleallowsindividualstomeasurethedistancebetweentwolocations.Then,askafewgroupsofstudentstosharethenumberofpacestheywrotedownontheirmaps.Whenstudentsnoticethatthenumberofpacesvariedwitheachgroup,askthemwhytheythinkthisis.Besuretoexplainhowrealmapsmeasurescaleinmetersorotherunitsforthesakeofaccuracyandconsistency.
3. LandformReview:Tellthestudentsthatamapcanrepresentvariouscomponentsoftheworld;someofthesecomponentsincludelandforms.Sincestudentsstudiedlandformsingrade2,theteachershouldbesuretoreviewthevarioustypesoflandforms.Theteachercanaskstudentsaboutanytypesoflandformstheyrememberandsomeoftheircharacteristics.Then,watchthevideo“WhatareLandforms?”Afterthestudentswatchthevideo,theteachercanaskthestudentstocompletethelistontheboard,usingtheinformationprovidedinthevideo.Hereisalinktothevideo:
a. https://www.youtube.com/watch?v=v48SV4zU9AkThevideocanbestoppedat2:00sincetherestofitisaquiz.
4. PhysicalMapInvestigationa. Presentaflatmapandatopographicalmaptothestudents
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b. Askthemtorespondtothequestion“Whatdobothmapshaveincommon(landforms,bodiesofwater)?c. Then,dividethestudentsintogroupsandletthegroupsobservethetwomapsandnotethedifferences
betweenthem.AskthemtorecordtheirfindingsintheirsciencejournalsbymakingaVenndiagram.d. Then,gatherthestudentsandaskthemtosharetheirfindingswiththeclass.Theteachershouldmakeagiant
Venndiagramontheboardsothatstudentscanseethedifferencesandsimilaritiesbetweenthemaps.
5. OnlineMaps:GiveeachstudentadeviceandhavethemexploreGoogleEarthsotheycanlookatpicturesoftheEarth,startinginNorthAdams,thenhavethemcompletetheGoogleEarthworksheet.
6. Forthislesson,studentswillcreateaphysicalmapofMassachusetts.AblanktemplateofMassachusettswillbeprovidedfortheclassroomteachertocopyandhandouttostudents.(SP2:Developingandusingmodels)
a. Thereareseveralitemsthatabasicmapincludes.Talktothestudentsaboutwhatamaphas,includingatitle,alegend,acompassrose,boundaries,color,labelsetc.Alltheseitemsshouldbeincludedinthemapsthestudentscreate.
b. Studentsshouldcreatealegendfortheirmaps.Thelegendmayincludecolorsandshapes.Forexample,theAppalachianMountainsrunthroughthewesternpartofMassachusetts.Thestudentsmaywanttodrawatriangletoindicateamountainintheirlegend.Then,drawafewtrianglesalongtheleftsideofMassachusettstorepresentthemountainrange.ThestudentsmayopttodrawatrianglethatisadifferentcolorandsizethentheresttorepresentMt.Greylock,thetallestmountaininMassachusetts.OntherightsideofMassachusetts,thestudentsmaywanttocolortheborderbluetorepresenttheAtlanticOcean.
AssessmentStudentswillcreateaphysicalmapofMassachusetts.
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Lesson2:Mohs’HardnessScaleLESSONBACKGROUNDThislessonismeanttobeanintroductiontothecompositionoftheEarth’ssurface.Thetopicsintroducedinthislessonincludeminerals,rocks,andtheMohsHardnessScale.Thislessonismeanttolaythefoundationforthetopicsoferosionandweathering,whichareimportanttounderstandhowtheEarth’ssurfacechanges.ScienceContentBackgroundMineralsandRocksAmineralisaninorganicsolidwithadefinitechemicalcompositionandacrystallinestructureformedbygeologicalandnaturallyoccurringprocesses.Arockisacombinationofoneormoremineralsbutmayalsoincludeorganicremainsandmineraloids.Somerocksarepredominantlycomposedofjustonemineral.Therearethreetypesofrocks:igneous,metamorphic,andsedimentary.Sedimentaryrocksareformedfromparticlescalledsediment,whichincludesand,shells,pebbles,andotherfragmentsofmaterial.Thesedimentaccumulatesinlayersandoveralongperiodoftimesolidifiesintorock.Sedimentaryrockistypicallysoftandmaybreakapart/crumbleeasily.Sedimentaryrocksareusuallytheonlytypethatcontainsfossils.MetamorphicrocksareformedunderthesurfaceoftheEarthfromthechange(metamorphosis)thatoccursduetointenseheatandpressure.Therocksthatresultfromtheseprocessesmayhaveshinycrystals,formedbymineralsgrowingslowlyovertime.Igneousrocksareformedwhenmagmacoolsandhardens.MagmaiscomposedofmoltenrockandisstoredintheEarth'scrust.Lavaismagmathatreachesthesurfaceofourplanetthroughavolcanovent.Whenlavacoolsveryquickly,nocrystalsformandtherocklooksshinyandglasslike.Sometimesgasbubblesaretrappedintherock,leavingtheappearanceoftinyholes/spacesintherock.
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TheMohsHardnessScaleTheMohsHardnessTestisusedtoidentifyamineral.Thetestisusefulbecausemostspecimensofagivenmineralareveryclosetothesamehardness,whichmakeshardnessareliablediagnosticproperty.Thescalegoesfrom1-10,with1beingthesoftestmineral(talc).Fromsoftesttohardest,thescaleisasfollows:Talc,gypsum,calcite,fluorite,apatite,orthoclase,quartz,topaz,corundum,diamond.OverviewoftheLessonStudentswillusetheMohsHardnessScaletoperformtestsonacollectionofminerals.Theteachershouldcarefullyreadoverthelessonbeforeteachingthislessoninordertogainabetterunderstandingoftheconceptstheywillneedtoexplaintothestudents.StudentswillbecreatingachartaboutthemysterymineralsanddesignanadfortheirDailyPlanetEarthNewspaperproject.FocusandSpiralStandardsFocusStandard:4-ESS1-1.Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.ClarificationStatement:
• Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.
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StateAssessmentBoundary:• Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrock
formationsandlayers.• Assessmentislimitedtorelativetime.
SpiralStandard:3-LS4-1.Usefossilstodescribetypesoforganismsandtheirenvironmentsthatexistedlongagoandcomparethosetolivingorganismsandtheirenvironments.RecognizethatmostkindsofplantsandanimalsthatoncelivedonEartharenolongerfoundanywhere.ClarificationStatement:
• Comparisonsshouldfocusonphysicalorobservablefeatures.StateAssessmentBoundary:
• Identificationofspecificfossilsorspecificpresent-dayplantsandanimals,dynamicprocesses,orgeneticsarenotexpectedinstateassessment.
SpiralStandard:6-MS-ESS1-4.Analyzeandinterpretrocklayersandindexfossilstodeterminetherelativeagesofrockformationsthatresultfromprocessesoccurringoverlongperiodsoftime.ClarificationStatements:
• Analysisincludeslawsofsuperpositionandcrosscuttingrelationshipslimitedtominordisplacementfaultsthatoffsetlayers.
• Processesthatoccuroverlongperiodsoftimeincludechangesinrocktypesthroughweathering,erosion,heat,andpressure.
StateAssessmentBoundary:• Stratasequencesthathavebeenreorderedoroverturned,namesofspecificperiodsorepochsandeventswithinthem,
ortheidentificationandnamingofmineralsorrocktypesarenotexpectedinstateassessment.SpiralStandard:6-MS-ESS2-3.Analyzeandinterpretmapsshowingthedistributionoffossilsandrocks,continentalshapes,
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andseafloorstructurestoprovideevidencethatEarth’splateshavemovedgreatdistances,collided,andspreadapart.ClarificationStatement:
• Mapsmayshowsimilaritiesofrockandfossiltypesondifferentcontinents,theshapesofthecontinents(includingcontinentalshelves),andthelocationsofoceanstructures(suchasridges,fracturezones,andwedges),similartoWegener’svisuals.
• StateAssessmentBoundary:Mechanismsforplatemotionorpaleomagneticanomaliesinoceanicandcontinentalcrustarenotexpectedinstateassessment.
LearningTargetsIcanperformappropriateteststodeterminethehardness,color,luster,cleavage,andstreakofdifferentminerals.Icannotedifferencesbetweenrocksandminerals.Icanusepreviouslyrecordeddatatoidentifydifferentminerals.Assessments
● Studentswillcreateachartoftheirobservationsofdifferentminerals.● Studentswillusealistofcharacteristicsgiventothemtoidentifythemysterymineralsquartzandlimestone.● Aspartoftheportfolionewspaperproject,studentswillbecomeanexpertononeofthemineralstheyobservedand
createanadvertisementforthismineral.
TargetedAcademicVocabularyTier1:colorTier2:organic,hardness,streakTier3:mineral,crystal,luster,cleavage,igneousrocks,sedimentaryrocks,metamorphicrocks
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RESOURCESANDMATERIALSQuantity Item Source
1perstudent HandLens Bin
5Whiteand5Blackplates(1pergroup)
Streakplates Bin
5pergroup Penny Bin
5pergroup Nail Bin
1boxperclass MineralKit-Includes15mineralsamples Bin
1perpair/group Limestonesample Bin
1perpair/group Quartzsample Bin
1perstudent ScienceJournal ClassroomTeacher
RockCleavageVideohttps://www.youtube.com/watch?v=zAOTfSWjw0Q&list=PLsAWD8mKKE95eF864ryLNK8SXJfJ-EsWh&index=1
CMCWebsite
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1piece ChartPaper ClassroomTeacher
1 “HowtoDescribeLuster”Board Bin
1perstudent RocksandMineralsComparisonChart Binder
1perstudent MineralObservationChart Binder
1perstudent MCASquestion Binder
1 MineralsandRocksPowerPoint CMCWebsite
1perstudent GeoSquadComic Binder
1perstudent DailyPlanetEarthMineralAdvertisementTemplate CMCWebsite**Itemsinboldshouldbereturnedforusenextyear**LESSONDETAILSLessonOpening/Activator
1. TheEarthismadeupofmanydifferenttypesofminerals;somearemorecommonthanothers.Today,we’regoingtogoonamysterymineralhunttolearnmoreaboutwhatmineralsareandhowtoidentifythem.Besuretoexplainthedifferencebetweenrocksandminerals.Rocksaregroupsofdifferentmineralsthatformtogether.Therefore,mineralsmakeuprocks.
2. PresenttheMineralsandRocksPowerPointandthenshowtheMightyMineralsAnimation(includedinthePowerPoint).ThisismeanttobeanintroductiontotheGeoSquadcharacters:Izzy,Maggie,andSpencer.Then,showtheGeoSquadcomictostudents(thisisalsoincludedinthePowerPoint)havethestudentsfollowalong.Note:Theteacher
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willneedtomakecopiesoftheGeoSquadcomicsothatthestudentscanreadalong.3. Belowisachartthatcomparesmineralsandrocks.Theclassroomteachershouldmakecopiesofthistohandoutto
studentstopasteintheirsciencejournals.DuringtheLesson
1. PhysicalPropertiesofMinerals:Belowarethephysicalpropertiesofamineral:a. Describethefollowingterms,whileusingpart2ofthePowerPointasavisual.b. Colorissimplywhatcolorthemineralis.Studentswillidentifythisthroughobservation.c. Lusterishowshinyordullsomethingisandcanbeclassifiedusingthosewords.Lustercanalsobedescribedas
pearly,greasy/oily,earthy/dull,orwaxy.Studentstestlusterbyobservingtherocksanddescribingthewayitappearsinthelight.Examplesoflusterareprovidedontheboardthatsays“HowtoDescribeLuster”whichisincludedinthebin.
d. Cleavageishowthemineralbreaksintopieces.Somemineralsbreakupintochunksorsmallcubeswhileothersbreakupintosmallthinsheets.Cleavagecanbeobservedbylookingatthenumberofflat/curvedsidesonamineralandtheanglebetweenthem.Besuretotaketimetoexplainthisconcept,itmightbehelpfultoshowthefollowingvideohttps://www.youtube.com/watch?v=zAOTfSWjw0Q&list=PLsAWD8mKKE95eF864ryLNK8SXJfJ-EsWh&index=1
e. Streakisthecolorofpowderwhendraggedacrossanon-weatheredsurface.Inthistest,studentsscrapethemineralacrossablackstreakplateandawhitestreakplatetoseeifanycolorisleftontheplate.Forexample,whenwewritewithapencil,we’recreatingastreakfromthegraphite.
2. DescribingMinerals:Beforethehands-onactivity,theteachershouldtalktothestudentsabouteachmethodofdescribingamineral.Useexamplesorexplainthathardnessistheabilitytoscratchthesurfaceofthemineral.
a. Hardnesscanbetestedwithyourfingernail,apenny,andasteelnail.b. Ifthefingernailcanscratchit,thatmeansithasahardnesslessthan2.c. Ifyoucanscratchthemineralwithapennybutnotafingernailit’smostlikelya3.d. Ifyoucanscratchitwithasteelnailbutnotapennyitmostlikelywillbebetween3and5.
3. MohsHardnessScale:TalkabouttheMohsHardnessScaleandhowtoreadthescale.TheMohsHardnessScalewas
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developedtocomparethehardnessofcertainminerals.Thescalegoesfrom1to10where1isthesoftestmineral(orveryeasytoscratch)and10isthehardest(orverydifficulttoscratch).Anexampleofa1wouldbegraphite.Anexampleofa9and10wouldberubiesanddiamonds.Understandingthehardnessofamineralisimportantbecauseithelpspeopledeterminewhatthatmineralcouldbeusedforwhetheritbejewelry,carving,storage,etc.It’salsoveryhelpfulwhenidentifyingminerals.
a. UsethesampleMCASquestiontoshowstudentshowtheyshouldinterprettheMohsScale.Note:Memorizingthenumbersandmineralsisnotimportant,ratherthekidsshouldunderstandhowtointerpretthescaleandwhatthenumbersmean.i. ThecorrectanswerisA.apatitebecauseitisbetweenthefluorite(4)andquartz(7).Ifthemineral
scratchesfluoritethanitisatleasta4orhigher.Ifitdoesnotscratchquartzthanitcannotbeabovea7.Theonlymineralfromthelistofoptionsthatisbetween4and7isapatite.
4. MineralObservationStations:Dividestudentsintofivegroupsandgiveeachstudentamineralobservationcharttorecordinformationateachstation.Ateachofthefivestationssetupthreeminerals(fromthemineralkit)alongwithstreakplates,anail,andapenny.Givethestudentstimetoobserveonemineralateachofthestations.[ScientificPractice4AnalyzingandInterpretingData]Oncethestudentshavemadeandrecordedtheirobservations,comebacktogetherasaclassanddiscusswhattheysaw.Askthestudents:Whatdidyoufind?Weretheresometeststhatwereeasiertoperformthanothers?Whatwasdifficultaboutthisexperiment?**Ifthereisatimeconstraintthelessoncanbedividedintotwopartsbeginninghere.**
5. TheMysteryRockExperiment:Thisactivitycanbedonewithapartneroringroups.Givethestudentsasampleofquartzandlimestonewithouttellingthemwhattheyare.Havethestudentsidentifywhichmineraliswhichbyperformingthetests.Afterthisactivityiscompleteandthestudentshaveidentifiedthemineralsprovidesomebackgroundabouteachmineral,descriptionsaregivenbelow:
a. QuartzisthemostabundantmineralonEarth.Itisoftenahard(hardness=7onMohs),whiteorcolorlessmineralthatismadeofsilicondioxide.Althoughitismostoftenwhiteorcolorless,quartzcanalsobefoundinavarietyofenvironmentsandcolors.Itisfoundinigneous,metamorphic,andsedimentaryrocks.Typically,quartzisusedasgemstonesinjewelrybecauseitishardandcolorful.
b. Limestoneisasedimentaryrockcomposedofcalciumcarbonate.Limestoneisimpactedduetopressure.Itis
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veryhard,andthetexturecanbeverysmoothorcoarse.Themostcommonuseoflimestoneisforconstructionandarchitecture.ThepyramidsofGizaaremadeoflimestone.Itmayalsobeusedascountertopsandforbuildingfireplaces.
6. MineralAd:Studentswillnowcreateadsonthecomputersthatwillbeaddedtotheir“DailyPlanetEarth”newspapers.Theadswillbebasedononemineraltheyobservedfromthelesson.Remindthestudentsthatthepurposeoftheadvertisementistomakethemineralappealing,sothatthereaderswillwanttobuyit.Eachadvertisementshouldexplicitlystatethemineraltypeandincludesomeofthemineral’squalities.Furthermore,studentsshouldincludeatleastoneimageoftheirmineral.Somequalitiesthatstudentscanincludeintheiradsare:• Luster• Color• Hardness• Shape• Size• Uses• Crystalstructure
***Studentswillcreatetheiradvertisementsandcopyandpastetheirimagesintothenewspapertemplate.Assessments
● Studentswillcreateachartoftheirobservationsofdifferentminerals.● Studentswillusealistofcharacteristicsgiventothemtoidentifythemysterymineralsquartzandlimestone.● Aspartoftheportfolionewspaperproject,studentswillbecomeanexpertononeofthemineralstheyobservedand
createanadvertisementforthismineral.
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Lesson3:WhatisErosion?
BACKGROUNDThislessonintroducestheconceptsofweatheringanderosioninpreparationforlessons4and5.Studentswilllearnabouthowrocksarebrokendownandmoveduntiltheyturnintosoil,andwillhaveabriefintroductiontofossils.ScienceContentBackgroundWeatheringanderosionareimportantprocessesthatgraduallyweardowndirtandleadtotheproductionofsoil.Weatheringbreaksrocksintosmallerandsmallerpiecesbutleavestheminplace,whereaserosionbreaksdownrocksbycarryingthemawayfromtheiroriginallocations.Weatheringanderosioncanworktogethertomakerocksdisappear;forexample,manyrocksareweatheredintosmallchunks,andthenthosechunksareerodedawayandbrokenintoevensmallerpiecesastheyarebeingmoved.Waterandlivingthingslikeplantsandmicroorganismsarethemaindriversofweathering.Themaindriversoferosionarewaterandwind.WateristhemaincauseoferosiononEarth,whetherit’sinliquidorsolidform.Inliquidform,watercancarryawaypiecesofrockwhilemovinginariver,flood,orwave.Insolidform,itmovesdirtandrockasaglacier.Weatheringanderosionturnrocks,aswellasentirelandformsmadefromrocks,intogravel,andsandyandclay-likedirt.Plants,microorganisms,andanimalslikewormsusethisdirtandchangeitintodark,fertilesoil;inotherwords,theyactasadecomposerintheirsoilhabitat.Becauseallthesoil,sand,andgravelintheworldwasatonetimeapartofarock,dirttypesaredifferentbasedonwhichmineralswereintherockstheycamefrom.
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FocusandSpiralStandard(s)FocusStandard:4-ESS1-1.Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.ClarificationStatement:
• Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.
SpiralStandard:3-LS4-1.Usefossilstodescribetypesoforganismsandtheirenvironmentsthatexistedlongagoandcomparethosetolivingorganismsandtheirenvironments.RecognizethatmostkindsofplantsandanimalsthatoncelivedonEartharenolongerfoundanywhere.ClarificationStatement:
• Comparisonsshouldfocusonphysicalorobservablefeatures.StateAssessmentBoundary:
• Identificationofspecificfossilsorspecificpresent-dayplantsandanimals,dynamicprocesses,orgeneticsarenotexpectedinstateassessment.
SpiralStandard:6.MS-ESS1-4.Analyzeandinterpretrocklayersandindexfossilstodeterminetherelativeagesofrockformationsthatresultfromprocessesoccurringoverlongperiodsoftime.ClarificationStatements:
• Analysisincludeslawsofsuperpositionandcrosscuttingrelationshipslimitedtominordisplacementfaultsthatoffsetlayers.
• Processesthatoccuroverlongperiodsoftimeincludechangesinrocktypesthroughweathering,erosion,heat,andpressure.
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StateAssessmentBoundary:• Stratasequencesthathavebeenreorderedoroverturned,namesofspecificperiodsorepochsandeventswithinthem,
ortheidentificationandnamingofmineralsorrocktypesarenotexpectedinstateassessment.SpiralStandard:6.MS-ESS2-3.Analyzeandinterpretmapsshowingthedistributionoffossilsandrocks,continentalshapes,andseafloorstructurestoprovideevidencethatEarth’splateshavemovedgreatdistances,collided,andspreadapart.ClarificationStatement:
• Mapsmayshowsimilaritiesofrockandfossiltypesondifferentcontinents,theshapesofthecontinents(includingcontinentalshelves),andthelocationsofoceanstructures(suchasridges,fracturezones,andtrenches),similartoWegener’svisuals.
StateAssessmentBoundary:• Mechanismsforplatemotionorpaleomagneticanomaliesinoceanicandcontinentalcrustarenotexpectedinstate
assessment.FocusStandard:4-ESS2-1.Makeobservationsandcollectdatatoprovideevidencethatrocks,soils,andsedimentsarebrokenintosmallerpiecesthroughmechanicalweatheringandmovedaroundthrougherosion.ClarificationStatements:
• Mechanicalweatheringprocessescanincludefrostwedging,abrasion,andtreerootwedging.Erosioncanincludemovementbyblowingwind,flowingwater,andmovingice.
StateAssessmentBoundary:• Chemicalprocessesarenotexpectedinstateassessment.
SpiralStandard:2-ESS2-4.ObservehowblowingwindandflowingwatercanmoveEarthmaterialsfromoneplacetoanotherandchangetheshapeofalandform.ClarificationStatement:
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• Examplesoftypesoflandformscanincludehills,valleys,riverbanks,anddunes.SpiralStandard:7.MS-ESS2-2.ConstructanexplanationbasedonevidenceforhowEarth’ssurfacehaschangedoverscalesthatrangefromlocaltoglobalinsize.ClarificationStatements:
• Examplesofprocessesoccurringoverlargespatialscalesincludeplatemotion,formationofmountainsandoceanbasins,andiceages.
• Examplesofprocessesoccurringoversmall,localspatialscalesincludeearthquakesandseasoningweatheringanderosion.
Science/EngineeringPractice(SP) DisciplinaryCoreIdea(DCI) CrossCuttingConcepts(CCC)
● PlanningandCarryingOutInvestigations
● Planningandcarryingoutinvestigationstoanswerquestionsortestsolutionstoproblemsin3–5buildsonK–2experiencesandprogressestoincludeinvestigationsthatcontrolvariablesandprovideevidencetosupportexplanationsordesignsolutions.
● Makeobservationsand/ormeasurementstoproducedatato
ESS2.A:EarthMaterialsandSystemsRainfallhelpstoshapethelandandaffectsthetypesoflivingthingsfoundinaregion.Water,ice,wind,livingorganisms,andgravitybreakrocks,soils,andsedimentsintosmallerparticlesandmovethemaround.(4-ESS2-1)ESS2.E:BiogeologyLivingthingsaffectthephysicalcharacteristicsoftheirregions.(4-ESS2-1)
CauseandEffectCauseandeffectrelationshipsareroutinelyidentified,tested,andusedtoexplainchange.(4-ESS2-1), (4-ESS1-1)
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serveasthebasisforevidenceforanexplanationofaphenomenon.(4-ESS2-1)
LearningTargets
1. Icanobserveanddescribeexamplesofweatheringthroughfrostwedging,abrasionandtreerootwedging.2. Icanobserveanddescribeexamplesoferosionthroughwind,water,andice.3. Icanexplainthedifferencebetween“weathering”,“erosion”,and“deposition”.
AssessmentStudentswillcreateanarticleabouterosiononMt.Greylockfortheir“DailyPlanetEarthNewspaper.”StudentswilltypeuptheirarticlesandincludeimagesoftheeffectsoferosiononMt.Greylock.Intheirarticles,studentsshouldfirstdescribeMt.Greylock,specifically,theminerals/rockswhichmakeupMt.Greylock(theylearnedinlesson2thatitiscomposedofquartzandlimestone)Thestudentsshouldalsowriteabouttheerosionprocessbasedonwhattheylearnedinthelesson.Studentswilltypetheirarticlesandcopyandpastetheirinformationintothenewspapertemplate.WIDALanguageObjectives(DependentontheneedsofyourELLstudents)TargetedAcademicLanguage/KeyVocabulary
Tier3:frostwedging,abrasion,treerootwedging,erosion,weathering,deposition
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RESOURCESANDMATERIALS
Quantity Item Source
1perclassroom Computer+projector ClassroomTeacher
1perclassroom Weathering&ErosionPowerPoint CMCWebsite
1perclassroom ActivityStationSetup(Rock&Roll,andSweptAway:HandsonNaturep.253-254(eachofthesestationsrequirenumerousmaterials,besuretousecornmealforthesweptawaystationratherthanrice)
Binder
What’sStrongEnoughtoMakeaCanyon?https://tinyurl.com/ybzlhu2g) CMCWebsite
1pergroup Stickytack Bin
2(1perSplashstation;1perSweptstation)
Bakingpan Bin
1perSplashstation Tablespoon Bin
2perstudent 3oz.Dixiecups Bin
1perstudent Spoon Bin
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1pergroup Paperplateandplasticplate Bin
Asneeded Cinnamon Bin
Asneeded Salt Bin
1pergroup 2binderclips Bin
1pergroup 2plasticcups Bin
1pergroup 1plasticcondimentcontainer Bin
1pergroup Ruler ClassroomTeacher
1setperclassroom LaminatedImagesofBerkshireLandforms Bin
Asneeded Water ClassroomTeacher
2perRockstation Clean,sealableplasticcontainer Bin
3handfuls(2perRockstation;1perSweptstation)
Stones Bin
1perclassroom Smallbagofcornmeal Bin
1handfulperSweptstation Blocksofwood Bin
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1perstudent Straws Bin
1perstudent “PreparingforDisaster”reading Binder
1perstudent “WatchforSteadyRocks”reading Binder
1perstudent PairedTextQuestionsWorksheet Binder
10 Smallplasticdinosaurs Bin**Itemsinboldshouldbereturnedforusenextyear**LessonPrepThenightbefore,placepiecesofsandandgravelinanicetray,fillitwithwater,andfreezethe“gravelicecubes”fortheglacierdemo.GatherthematerialsusedintheRock&RollactivityandtheBlownAwayactivityandreviewtheCanyonactivity(availableathttps://tinyurl.com/ybzlhu2g)andputtogetherthedripsticks.LESSONDETAILSLessonOpening/ActivatorUsetheWeatheringandErosionPowerPointtoguidethisdiscussion.
1. ShowthefirstimageinthePowerPoint(rootwedging)andaskforvolunteerstoguesswhatishappeninginthepicture.Toguidethestudents,askprobingquestions:Whyaretheobjectsinthispicturewheretheyare?Doyouthinkanythingisbeingmoved,pushed,orchangedinsomeway,evenifitishappeningslowly?Whatisdoingthemovingandchanginginthispicture?Whatdoyouthinkthisimagelookedlikeinthepast?Whatdoyouthinkitwilllooklikeinthefutureifthesameactionkeepshappening?
2. AttheendofthePowerPoint,takesometimetoclarifythedifferencebetween
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weathering,erosionanddeposition.(Weatheringbreaksrocksintosmallerpiecesbutleavestheminplace;erosionmovesthesesmallpieces,aswellassoil,awayfromoneplace;depositionpilesupthosepiecesinadifferentlocation.)ThePowerPointalsoasksabouttheendresultsofweatheringanderosion;thestudentsshouldunderstandthatwhenrocksgetbrokenupintosmallenoughpiecesandcarriedaway,theybecomesoil,sand,anddirt.
DuringtheLesson
1. ErosionandAbrasionStationsa. Thefollowingtwostationsshouldbesetupoutside,ifpossible.Breaktheclassintotwogroups.Using“Handson
Nature,”setuptwoactivitystations:Rock&Roll(weatheringbyabrasion)andSweptAway(erosionbywind).InSweptAway,substitutedrycornmealfortherice.Theinstructionscanbefoundonpages253-254of“HandsonNature.”[SP2:UsingModels].Itwouldbeidealtohaveoneadultateachstation.Dividethestudentsintogroupsandhavethemspendaround10-15minutesateachstation.
2. WashingAwayLandforms
a. Setupthematerialsforthe:“What’sStrongenoughtoMakeaCanyon?”lesson,availableathttps://tinyurl.com/ybzlhu2g,using6or8cupsofcornmealinsteadof4.However,insteadofplacingadripstickoverthecornmealland,theteacherwillplaceagravelcubeonthecornmeal.Astheicecubemelts,itwillslidedownthecornmeal,creatingatiny“valley”andleavingbehindlittlepiecesofgravel.Havethestudentswatchtheicecubeforalittlewhileandaskthemifthismodelremindsthemofanytypeoferosiontheyhavelearned.Guidethestudentsintounderstandingthatthismodelresemblesthemovementofglaciers.
b. Breakeachofthegroupsoftwoorthreeandcompletethecornmealactivity.Insteadofhavingeverygroupmakeaflatpieceofland,however,assignsomegroupstosculptamountain,somegroupstobuildavalley,somegroupstomakeacrater,andsomegroupstomakeaflatplainasspecifiedbytheactivity.TheteacherandScienceFellowcangoaroundhelpingthestudentsasneededinsculptingtheirlandformsusingspoonsandcups.Findthreegroupsandaskthemtohideoneplasticdinosaurintheircornmealland.
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c. (LetthestudentsvoiceandsharetheirideasusingtheA/Btalkingprotocol).Attheendoftheactivity,haveeachgroupvisitastationthathadadifferentlandformfromtheirown.Asaclass,discusshowsimilaritiesanddifferencesinthewaydifferentlandformseroded.Askthestudentsifanyofthemnoticedthedinosaursinsidetheland.Tellthemthattheserepresentthefossils,whicharetheancientbonesofthedinosaursthathavebeenburiedovertime.Askthestudentsiftheythinkerosionhelpsuslearnaboutthepastandhow.
3. BerkshireLandforms
a. SplitthestudentsintogroupsandpassouttheimagesofBerkshirelandforms.Havethemlookovertheimagesandmakenotesintheirsciencejournalsofwheretheyseeerosioninthepictures.Thestudentsshouldexchangecardswithanothergrouponcethey’vehadafewminutestolookovertheimages.
LessonClosingTelleachgrouptoturnovertheirimageandfigureoutwhethertheirlandformwasmetamorphicorsedimentary.Then,makeachartontheboarddividingtherocksinto“Maggie”rocksand“Spencer”rocks,andhavestudentsaddtheirlandformstothechart.Remindthestudentsthatsedimentaryrocksoftencomefromtheoceanfloor,andmetamorphicrocksoftencomefrommountains.OptionalExtension
1.PairedPassagesActivitya. ThisisanoptionalactivitythatmaybecompletedwhentheScienceFellowsarenotpresent.
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b. Inthisexercise,studentswillreadtwopassagesandthencompareandcontrastthetexts.Afterreadingthetexts,thestudentswillthencompletethePairedTextQuestionsworksheet,whichtestsforcomprehension.Thetextsforthislessonare“WatchforSteadyRocks”and“PreparingforaDisaster”(locatedinthebinder).
AssessmentStudentswillcreateanarticleabouterosiononMt.Greylockfortheir“DailyPlanetEarthNewspaper.”StudentswilltypeuptheirarticlesandincludeimagesoftheeffectsoferosiononMt.Greylock.Intheirarticles,studentsshouldfirstdescribeMt.Greylock,specifically,theminerals/rockswhichmakeupMt.Greylock(theylearnedinlesson2thatitiscomposedofquartzandlimestone)Thestudentsshouldalsowriteabouttheerosionprocessbasedonwhattheylearnedinthelesson.Studentswilltypetheirarticlesandcopyandpastetheirinformationintothenewspapertemplate.
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Lesson4:WhatisaSoil?IsAllSoiltheSame?LessonBackgroundThislessonisfocusedonthetypesofsoil,soilcompositionandthecharacteristicsofsoil.ItiscriticalforthestudentstounderstandthatsoilisanimportantcomponentofthesurfaceoftheEarth.Learningmoreaboutsoilwillallowstudentstodeepentheirunderstandingoftheprocessesoferosion,weatheringanddepositionsincesoilisformedthroughthoseprocesses.ScienceContentBackgroundSoilistheupperlayeroftheEarthsurfacemadeupoffivedifferentelements:Inorganic,Microorganisms,Organic,WaterandAir (IMOWA). Generally, “ideal” soil ismade up of 45% inorganicmatter, 25% air, 25%water and 5%organicmatter andmicroorganisms.
OverviewoftheLessonThestudentswilllearnthecomponentsofsoilbyfirstobservingsoiloutside.StudentswillparticipateinadiscussionaboutsoilcompositionandwillusetheIMOWAcharttoguidethisdiscussion.Thestudentswilllearnthecharacteristicsofsoilandwillexplorethemusingthesoildrainagetest.FortheDailyPlanetEarthnewspaper,studentswillbecreatingarecipeforsoil.FocusandSpiralStandardsFocusStandard:4-ESS1-1.Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.ClarificationStatement:
• Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthe
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wallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.StateAssessmentBoundary:
• Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrockformationsandlayers.Assessmentislimitedtorelativetime.
SpiralStandard:3-LS4-1.Usefossilstodescribetypesoforganismsandtheirenvironmentsthatexistedlongagoandcomparethosetolivingorganismsandtheirenvironments.RecognizethatmostkindsofplantsandanimalsthatoncelivedonEartharenolongerfoundanywhere.ClarificationStatement:
• Comparisonsshouldfocusonphysicalorobservablefeatures.StateAssessmentBoundary:
• Identificationofspecificfossilsorspecificpresent-dayplantsandanimals,dynamicprocesses,orgeneticsarenotexpectedinstateassessment.
SpiralStandard:6.MS-ESS1-4.Analyzeandinterpretrocklayersandindexfossilstodeterminetherelativeagesofrockformationsthatresultfromprocessesoccurringoverlongperiodsoftime.ClarificationStatements:
• Analysisincludeslawsofsuperpositionandcrosscuttingrelationshipslimitedtominordisplacementfaultsthatoffsetlayers.
• Processesthatoccuroverlongperiodsoftimeincludechangesinrocktypesthroughweathering,erosion,heat,andpressure.
StateAssessmentBoundary:• Stratasequencesthathavebeenreorderedoroverturned,namesofspecificperiodsorepochsandeventswithinthem,
ortheidentificationandnamingofmineralsorrocktypesarenotexpectedinstateassessment.
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SpiralStandard:6.MS-ESS2-3.Analyzeandinterpretmapsshowingthedistributionoffossilsandrocks,continentalshapes,andseafloorstructurestoprovideevidencethatEarth’splateshavemovedgreatdistances,collided,andspreadapart.ClarificationStatement:
• Mapsmayshowsimilaritiesofrockandfossiltypesondifferentcontinents,theshapesofthecontinents(includingcontinentalshelves),andthelocationsofoceanstructures(suchasridges,fracturezones,andtrenches),similartoWegener’svisuals.
StateAssessmentBoundary:• Mechanismsforplatemotionorpaleomagneticanomaliesinoceanicandcontinentalcrustarenotexpectedinstate
assessment.LearningTargetsIcanexplainhowsoilisformedthroughdecompositionandweathering.Icanillustratetheconnectionbetweensoilformation(e.g.ratiosoforganicmattertominerals)anditscolorandtexture.Icanidentifyanddescribethedifferencesbetweensoil,loam,andclay.NGSSAlignmentScience/EngineeringPractice(SP) DisciplinaryCoreIdea(DCI) CrossCuttingConcepts(CCC)
PlanningandCarryingoutInvestigations:Planningandcarryingoutinvestigationstoanswerquestionsortestsolutionstoproblemsin3–5buildsonK–2experiencesandprogressestoincludeinvestigationsthatcontrol
ESS2.E:BiogeologyLivingthingsaffectthephysicalcharacteristicsoftheirregions.(4-ESS2-1)
Patterns can be used as evidence tosupportanexplanation. (4-ESS1-1), (4-ESS2-2)
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variablesandprovideevidencetosupportexplanationsordesignsolutions.Makeobservationsand/ormeasurementstoproducedatatoserveasthebasisforevidenceforanexplanationofaphenomenon.(4-ESS2-1)Assessment
● Studentswillbeassessedontheirknowledgeofhowsoilisformedthroughthe“soilrecipe”activity.● Toassesstheirknowledgeoforganicandinorganicmaterialaswellasitsconnectiontosoilformation,reviewscience
journals.Studentsshouldbecreatingan“IMOWA”chartandwritingasentenceortwoabouttheirobservationsofthesoilsamplethattheyareexploring.
WIDALanguageObjectives(DependentontheneedsofyourELLstudents)TargetedAcademicLanguage/KeyVocabulary
Tier1:soil,clay,loam,sandTier2:texture,particlesTier3:decomposition,decaying,organic,inorganic
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RESOURCESANDMATERIALSQuantity Item Source
2cupsperstudent
SoilfromDecayingMatter Bin
1perstudent Woodenskewers Bin
Asneededtocoverdesks
Newspaper ClassroomTeacher
1perstudent HandLens Bin
2perclass Sieve Bin
1perstudent ScienceJournal ClassroomTeacher
1piece Chartpaper ClassroomTeacher
15(3pergroup)
SodaBottles(funnel,planter,screen) Bin
15cups(3cupspergroup)
Sand Bin
15cups(3cups Pottingsoil Bin
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pergroup)
15cups(3cupspergroup)
Clay Bin
Asneeded Water ClassroomTeacher
5(1pergroup)
Measuringcup Bin
1 SpencerPowerPoint CMCWebsite
1 DailyPlanetEarthSoilRecipeTemplate CMCWebsite
1 IMOWAChart Binder**Itemsinboldshouldbereturnedforusenextyear**
LESSONDETAILSLessonOpening/Activator
1. SoilExploration:Dividethestudentsinsmallgroupsandsharewiththemthattheywillbestudyingthecompositionofthesoiloutontheplayground.Tellthemthattheyneedtorecordthedifferentelementstheyseeinthesoil.Givethestudents10-20minutestoexploresoiloutonandaroundtheplaygroundandthen,bringthestudentsbacktotheclassandaskthemsharetheirfindingswiththeclass.RemindthestudentsthatthesurfaceoftheEarthholdslotsofsoilandthatSpencerthesedimentaryrockfromthe
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GeoSquadwillbetellingthemmoreaboutsoiltoday.GothroughtheSpencerSedimentaryPowerPointonsoilwiththestudents.
DuringtheLessonIMOWAChart
2. Afterthesoilexploration,introducethestudentstotheIMOWAchart.Beforeyoubegin,distributetheIMOWAworksheet.Besuretoclarifythemeaningoforganic,inorganic,microorganismanddecompositionwiththeclass.
a. Inorganicmaterialsarefoundinsoilandoftenaccountforabouthalfofthesoil’smakeup.Mostofthetimethisinorganicmaterialtakestheformofsand,silt,orclay.Wesometimesrefertothispartasthesoil“dirt.”Inorganicreferstosomethingthatdoesnotcomefromlivingmatter,suchasamineral.Explaintothestudentsthatsometimeswefindotherinorganicmaterialsinsoilsuchascoins,trash,paperwrappersfromfood,etc.TheseareNOTessentialitemsforcreatingsoil(andshouldn’tevenbeinthesoil)butsometimesthesethingsfindtheirwayintosoil.Thesearestillinorganicmaterialsbecausetheydonotcomefromlivingmatter.Tellthestudentsthatcoins,bottles,plasticbagsfindtheirwayintothesoilbecauseofpollutionandtheymayharmthesoilandtheorganismslivinginit.Mostoftheinorganicmattercomesfromtheweatheringanderosionofrocks.Someweatheringmayoccurrightwherethesoilforms,someoftheinorganicmattermaycomefromweatheringofotherrocklocationsnearby.
b. Organicmaterialcomesfromlivingmatter.Thisistheotherhalfofthesoil’smakeup.Manytimes,theorganicmaterialisintheformofplantandanimalresidue(forexample,manure,leavesthatfellofftrees,oranimalsthathavedied).Explainthatthemoreorganicmaterialinthesoil,the“richer”thesoilis(andthebetteritisforfarmingbecauseorganicmatterstoreslotsofnutrients).Todeterminetherichnessofsoil,wewillobservethe
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colorandtextureofthematerial.Isthesoildarkincolorandsoft/smoothtothetouch?Ifyes,thenthissoilhasmoreorganicmaterialthaninorganicmaterial.Ifthesoilislighterincolor,drier,androughthenitisnotasrichandprobablyhaslessorganicmaterial.
c. Tinylivingthingscalledmicroorganismsarefoundinthesoil.Mostofthetime,youwon’tbeabletoseethemicroorganisms,whicharetypicallyintheformoffungusorbacteria.
d. Optional:AskstudentstoclassifytheelementstheyfoundinthesoilduringthesoilexplorationactivityusingtheIMOWAchart.Then,askafewofthemtosharetheirclassification.
3. Decompositionreferstotheprocessofdecayingorrotting.Asorganicmaterialismixedintosoilovertime,thosematerialsbegintodecayorrot.Afteralongtime,thematerialsarebrokendownsofinelythatyoudonotnoticetheminthesoil.
4. Explaintothestudentsthattherearedifferenttypesofsoilandthesedifferencescanbeduetothesoiltexture,colorandwaterretentioncapacity.Someexamplesofsoilare:sand,loam,clayandsilt.
a. Soilcolor:Thetypesofrockandorganicmatterthatarebrokendownresultindifferentsoilcolors.
b. Soiltexture:Theoriginalmaterialandtheextenttowhichtheoriginalmaterialhasbrokendown.Sandismadeupofsmallrockbits;clayismadeupoffinerrockbits;loamismadeupoflargerbitsofrockandorganicmaterial.
c. Waterretention:Becausesandhaslargerrockparticles,itcannotbepackedtogethertightlyandthereislotsofspaceinbetweengrainsofsand;waterisabletodrainthroughthesespaces.Clayismadeupoffineparticles
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thatfittogethertightly,withlittleairspace;therefore,itretainswaterwell.Loamhasalittlespaceinbetweenparticles;itisabletoretainwater,butnotasmuchasclay.
5. (Classdiscussion)SoilDiscoveryNote:Teachersneedtocomposesoilforthestudentstoobserveandsortthrough,itisimportanttogetagoodvarietyofmaterialsinthesoilsothatstudentsareabletogeneratealotofitemsontheir“IMOWA”charts.Itmaybehelpfultoaddinorganichuman-producedmaterialsaswellsuchasrubberbands,pencils,penniesorotherobjectsthatyoumayhaveintheclassroom,sokidsareabletonotethedifferencebetweenorganicandinorganicmaterial.Youcouldalsoaddnaturally-formingorganicmaterialssuchasrocksandminerals.
a. Layoutanewspaperortarpandgetstudentstorecordtheirpredictionaboutwhattheythinkisgoingtobeinthesoil,havethemwritetheirideasintheirsciencejournal.Aftertheyrecordafewthoughts,pourasampleofsoilontothenewspaperforthestudentstolook.Studentswilluseskewerstomoveparticlesaroundandtrytoseparatethesoilintopilesofsimilarparticles.Studentswillusethelensestoexaminefinerpiecesofthesoil.Asievecouldbeusedtoseparatesandfromfinersoilforstudentstoinspect.Havethestudentsfeelthesoilbetweentheirfingerssotheyareabletoexaminetexture.Studentswillrecordwhattheydiscoveredinthesoilsamplewithafewsentencesintheirsciencejournals.Thestudentsshouldseparatetheirfindingsintoanew“IMOWA”chartsotheycangraspthedifferencesbetweenthefourtypesofmaterials.Askstudentsiftheycanmakeaclaimastowhetherthereismoreinorganicororganicmaterialandaskthemtoprovidereasoningandevidencefortheirclaim.[SP7Engaginginargumentfromevidence]
6. SoilRecipeforNewspaperProject:Studentswillnowwriteasoilrecipefortheir“DailyPlanetEarth”Newspaper.First,studentsshouldfillintheingredients’columnwhichshouldincludesand,smallrocks,deadleaves,orotheritems
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studentsobservedintheirsoilsample.Studentsmayalsoincludebacteria,microorganisms,andmacroorganismslikewormsintheiringredients’list,butit’snotrequired.Next,studentswillwritethesoilrecipe’ssteps.
7. Therecipestepsare:a. Breakdownrocksintopieces.b. Then,breakdownotherorganicmaterial(deadleaves,flowers,bugs,etc.)c. Next,mixtheingredientsforalongperiodoftimetomimictheprocessofweatheringanderosion.(Theamount
ofstirringtimecanbedecidedbythestudent.)
***Studentswilltypetheirrecipesandcopyandpastetheirimagesintothenewspapertemplate.
4. SoilDrainageTest(thiscanbedoneinsmallgroupsorasaclass)[SP3-carryingoutaninvestigation]
a. Inthisactivity,studentswillexplorethecharacteristicsofthreetypesofsoili.e.color,textureandwaterretentioncapacity.
b. Inthebin,therearethreesodabottles,cutintwopieces:oneisfunnel-shaped,theotherlookslikeaplanter.Coverthetipwiththescreen(tightenwitharubberband)andplacethefunneltip-downintotheplanter.(Itmayhelptodothisexperimentovernewspaperforeasycleanup.)
c. Fillonefunnelwithdrysand,onewithloam(pottingsoil),andonewithclay.Taketimetoobserveanddescribeeachtypeofsoil,payingspecialattentiontocolorandtexture.Askthestudentstodrawadiagramoftheapparatusintheirsciencejournalsandwritedownwhichsoiltheythinkwillholdthemostwater
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d. Studentsmaysharetheirhypothesiswiththeclass.
e. Slowlypour1cupofwaterintoeachfunnel.Watchasthewaterfiltersthroughthesoilandintothebottomoftheplanter.
f. Nexthavestudentsdrawadiagramwiththeresultsoftheexperiment.Anexampleofwhattheentryshouldincludeisbelow.
g. Askwhichsoilwouldbebestforplants.Why?Assessment
● Studentswillbeassessedontheirknowledgeofhowsoilisformedthroughthe“soilrecipe”activity.● Toassesstheirknowledgeoforganicandinorganicmaterialaswellasitsconnectiontosoilformation,reviewscience
journals.Studentsshouldbecreatingan“IMOWA”chartandwritingasentenceortwoabouttheirobservationsofthesoilsamplethattheyareexploring.
ExtensionConnectionstoMountGreylockAskthestudents,howweatheringanderosionimpactthesoilonMt.Greylock?Howdoesthesoilmovefromthetopofthemountaintothebottom?Doesthesoilchangeorlookdifferentovertimeduetoweatheringanderosion?
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Lesson5:FoolingwithFossilsLESSONBACKGROUND
Studentsmustfirstlearnwhatafossilis.Fossilsprovideavaluablerecordofplantandanimallifeaswellasenvironmentalconditionsfrommillions,evenbillionsofyearsago.Remainsandtracesofancientlifearepreservedinrocksasfossils.ThefossilrecordisanaturaldocumentationoftheevolutionandhistoryoflifeonEarth.Itisimportanttonotethattherearemanydifferenttypesoffossils,butforthisunitwearefocusingonbodyfossils,tracefossils,andmoldfossils.ScienceContentBackgroundFossilstakemillionsofyearstoformastheyareembeddedintothesedimentaryrockthatisformedinthecrustoftheearth.Therearethreetypesoffossilsthatwewillbelearningabout:bodyfossils,tracefossils,andmoldfossils.Bodyfossilsarefossilsoftheactualorganismsthemselvesfoundintheearth;theseareorganismssuchasdinosaurbonesorpetrifiedwood.Tracefossilsareimpressionsoffossilsthatrepresenttoanatomyoftheorganism.ItisNOTacastoftheorganismitself,butinsteadrelatestohowitliveditslife;thesearefindingssuchasfootprints,burrows,oreggnests.Theyshowhowtheorganismmovedandwentaboutdailylife.Amoldfossilisafossilthatisanimpressionormoldoftheorganismitself.Theorganismlayinthesedimentforlongenoughthattherockaroundithardened,creatinganimpressionoftheorganism.Theorganismwasthenimpactedbyanotherfactorsuchaserosionandweathering,oranotherorganismthatateitaway,sothatallthatisleftisamoldoftheoriginallivingbeing.Thesearethethreemaintypesoffossilsthatarcheologistsworkwithintheirworkandwhatwewillbelookingattoday.
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OverviewoftheLessonStudentswillbemakingtheirownfossilsafterlearningaboutthethreedifferenttypesoffossils.Finally,studentswillbeaddingtotheirnewspaperportfolioswithanarticleaboutthefossilthattheymadeduringclass.NGSSAlignmentTableScience/EngineeringPractice(SEP) DisciplinaryCoreIdeas(DCI) CrossCuttingConcepts(CCC)
(4-ESS2-1) Analyzing and Interpreting Data Analyzing data in 3–5 builds on K–2 experiences and progresses to introducing quantitative approaches to collecting data and conducting multiple trials of qualitative observations. When possible and feasible, digital tools should be used.
Analyze and interpret data to make sense of phenomena using logical reasoning.
ESS1.C: The History of Planet Earth
Local, regional, and global patterns of rock formations reveal changes over time due to Earth forces, such as earthquakes. The presence and location of certain fossil types indicate the order in which rock layers were formed.
Cause and effect relationships are routinely identified, tested, and used to explain change. (4-ESS2-1), (4-ESS3-2)
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FocusandSpiralStandards:FocusStandard:4-ESS1-1.Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.ClarificationStatement:
• Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.
• AssessmentBoundary:• Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrock
formationsandlayers.Assessmentislimitedtorelativetime.SpiralStandard:3-LS4-1.Analyzeandinterpretdatafromfossilstoprovideevidenceoftheorganismsandtheenvironmentsinwhichtheylivedlongago.ClarificationStatement:
• Examplesofdatacouldincludetype,size,anddistributionsoffossilorganisms.Examplesoffossilsandenvironmentscouldincludemarinefossilsfoundondryland,tropicalplantfossilsfoundinArcticareas,andfossilsofextinctorganisms.
AssessmentBoundary:• Assessmentdoesnotincludeidentificationofspecificfossilsorpresentplantsandanimals.Assessmentislimitedto
majorfossiltypesandrelativeages.SpiralStandard:6.MS-ESS1-4.Analyzeandinterpretrocklayersandindexfossilstodeterminetherelativeagesofrockformationsthatresultfromprocessesoccurringoverlongperiodsoftime.ClarificationStatements:
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• Analysisincludeslawsofsuperpositionandcrosscuttingrelationshipslimitedtominordisplacementfaultsthatoffsetlayers.
• Processesthatoccuroverlongperiodsoftimeincludechangesinrocktypesthroughweathering,erosion,heat,andpressure.
StateAssessmentBoundary:• Stratasequencesthathavebeenreorderedoroverturned,namesofspecificperiodsorepochsandeventswithinthem,
ortheidentificationandnamingofmineralsorrocktypesarenotexpectedinstateassessment.SpiralStandard:6.MS-ESS2-3.Analyzeandinterpretmapsshowingthedistributionoffossilsandrocks,continentalshapes,andseafloorstructurestoprovideevidencethatEarth’splateshavemovedgreatdistances,collided,andspreadapart.ClarificationStatement:
• Mapsmayshowsimilaritiesofrockandfossiltypesondifferentcontinents,theshapesofthecontinents(includingcontinentalshelves),andthelocationsofoceanstructures(suchasridges,fracturezones,andtrenches),similartoWegener’svisuals.
StateAssessmentBoundary:• Mechanismsforplatemotionorpaleomagneticanomaliesinoceanicandcontinentalcrustarenotexpectedinstate
assessment.LearningTargets:Icanwriteastoryaboutthehistoryofmyfossil.Icanexplainthedifferencesbetweentypesoffossils.
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AssessmentStudentswillwriteastoryaboutthefossiltheymadeinclasstoday.Thestoryshouldincludefactsaboutthefossilsuchaswhattypeoffossil,whereitcamefrom,andwhattimeperioditformed.Encouragethestudentstotellthestoryoftheirfossil.TargetAcademicLanguage:Tier2:PrehistoricTier3:Jurassic,Fossil
RESOURCESANDMATERIALSQuantity Items Source
6(twoofeachtype) Differenttypesoffossils Bin
1bag WholeWheatFlour Bin
2containers Salt Bin
1 Measuringcup(thatcanmeasureatleast1cup)
Bin
Variousitemstopressintosaltdoughtomakefossils
ClassroomTeacher/Outdoors
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1perstudent FossilHandout Binder(teachertomakecopies)
FossilPowerPoint CMCWebsite
DailyPlanetEarthFossilArticleTemplate CMCWebsite
Laptops/iPads ClassroomTeacher**Itemsinboldshouldbereturnedforusenextyear**
LESSONDETAILSLessonOpening/Activator
Studentswillbelookingatmoldsofmodelfossilsthattheteacherwillpassaround.Thestudentsareencouragedtotouchandfeelthesemodels,guessingwhattheyareastheypassthemaround.Theteacherwillleadadiscussionaboutwhattheyaretouchingandrevealthattheyarefossilsfrommillionsofyearsago.ThentheywillgooverthefossilPowerPointaboutthethreedifferenttypesoffossilsfoundinthisunit.
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DuringtheLesson:1. Makeyourownfossil:Studentswillbemakingtheirownfossilstodayfromsaltdough.
Thiswillneedtobemadeinadvancebytheteacher,thedirectionscanbefoundhere:https://www.makelifelovely.com/diy-dinosaur-fossils-with-salt-dough/Giveeachstudentaballofsaltdough.Thenhavethestudentsgooutsideandsearchforvariousnaturalitemstheycanpressintotheirsaltdoughtomakeafossil.
2. FossilMap:StudentswillnowbelookingatamapwiththeteacheroffossilsfoundallovertheworldbutshouldfocusspecificallyontheUnitedStatesanditregions.Theteachershoulddemonstratehowtousethewebsite,sostudentscanexploreitontheirowninsmallgroups.Pointoutdifferentregionsofthecountryandthendividethegroupsuptolookateach.Thiswillcoincidewiththeirsocialstudieswork.Thiswilltakepreparationwithunderstandingandfamiliarizingyourselfwiththewebsite.
a. https://paleobiodb.org/navigator/3. FossilStory:Studentswillnowwriteastoryaboutthefossilthattheyhavemade.They
willbepretendtheyarearchaeologiststellingtheworldabouttheamazingfossilthattheyhavejustdiscovered.Theirarticleshouldincludewhattheirfossilisandwhattype,wheretheyfoundit,howoldtheythinkitis,whattimeperiodit’sfrom,andhowitformed.Thiswillbeincludedasanarticleintheirnewspaperportfolio.
Extension:TakeafieldtriptotheBerkshiremuseum!IntheMuseumstudentscandigfordinosaurbonesandlookatrealfossilsintheprehistoricexhibits.
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OtherResource:Hereisawebsitethatlistsallthestatesandthefamousfossilsthathavebeenfoundinthem:https://www.fossilera.com/pages/state-fossilsLessonClosingStudentswhowanttopresenttheirfossilshouldbegiventheopportunitytodoso.Theteachershoulddoafinalreviewofthetypesoffossils.
AssessmentStudentswillwriteastoryaboutthefossiltheymadeinclasstoday.Thestoryshouldincludefactsaboutthefossilsuchaswhattypeoffossil,whereitcamefrom,andwhattimeperioditformed.Encouragethestudentstotellthestoryoftheirfossil.
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Lesson6:EarthquakesandFaultLines
LESSONBACKGROUND
Thislessoncoverstheeffectsoftectonicplatemovementincludingthecreationofvolcanoesandmountains.Majoractivitiesinthislessonincludesahands-oninvestigationofplatemovementaswellasaresearchprojectontheringoffire.
ScienceContentBackgroundThislessonisgroundedheavilyinplatetectonicsandtheeffectsofplatemovement,soteacherswillneedtounderstandanddemonstratetheseeffects.Tobegin,teachersmustunderstandthattheEarthismadeofmanylayers,theoutermostlayeroftheEarthiscalledthecrust.Thecrustisbrokenupintopiecesthatarecalledtectonicplates.Thislessoncoverstwotypesofboundariesthatoccurwhentectonicplatesinteractwitheachother.Theseboundariesarecalledtransformboundariesandconvergentboundaries.Atransformboundaryoccurswhentwotectonicplatesrubtogether.Asthepressurebuildsbetweentheplates,theyslipreleasingtheenergythatweperceiveasanearthquake.Aconvergentboundaryoccurswhentwotectonicplatescollidewitheachother.Asthetwoplatescollidetheyformmountainsbetweenthemasthelandshiftsupward.Thislessonalsocoversthecreationofvolcanoeswhichoccursatasubductionzone.Asubductionzoneoccurswhenadenseroceanicplateisthrustunderneathalessdensecontinentalplate.Apieceoftheoceanicplatebreaksoffandmeltsallowingformagmatocometothesurface.Thismagmahardensandformswhatweknowasavolcano.
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OverviewoftheLessonStudentswilllearnabouttheformationofvolcanoes,mountains,andearthquakesbyparticipatinginaseriesofexperimentsthatdemonstratetheeffectsofplatetectonics.FortheDailyPlanetEarthproject,studentswillbecreatinganewsarticleaboutanaturaldisasterthattheyresearch.FocusandSpiralStandardsFocusStandard:4-ESS2-2.AnalyzeandinterpretdatafrommapstodescribepatternsofEarth’sfeatures.[ClarificationStatement:MapscanincludetopographicmapsofEarth’slandandoceanfloor,aswellasmapsofthelocationsofmountains,continentalboundaries,volcanoes,andearthquakes.SpiralStandard:2-ESS2-2.Maptheshapesandtypesoflandformsandbodiesofwaterinanarea.ClarificationStatements:
• Examplesoftypesoflandformscanincludehills,valleys,riverbanks,anddunes.• Examplesofwaterbodiescanincludestreams,ponds,bays,andrivers.• Quantitativescalinginmodelsorcontourmappingisnotexpected.
SpiralStandard:6.MS-ESS2-3.Analyzeandinterpretmapsshowingthedistributionoffossilsandrocks,continentalshapes,andseafloorstructurestoprovideevidencethatEarth’splateshavemovedgreatdistances,collided,andspreadapart.ClarificationStatement:
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• Mapsmayshowsimilaritiesofrockandfossiltypesondifferentcontinents,theshapesofthecontinents(includingcontinentalshelves),andthelocationsofoceanstructures(suchasridges,fracturezones,andtrenches),similartoWegener’svisuals.
StateAssessmentBoundary:• Mechanismsforplatemotionorpaleomagneticanomaliesinoceanicandcontinentalcrustarenotexpectedinstate
assessment.SpiralStandard:7.MS-ESS2-2.ConstructanexplanationbasedonevidenceforhowEarth’ssurfacehaschangedoverscalesthatrangefromlocaltoglobalinsize.ClarificationStatements:
• Examplesofprocessesoccurringoverlargespatialscalesincludeplatemotion,formationofmountainsandoceanbasins,andiceages.
• Examplesofchangesoccurringoversmall,localspatialscalesincludeearthquakesandseasonalweatheringanderosion.
SpiralStandard:8.MS-ESS2-1.UseamodeltoillustratethatenergyfromEarth’sinteriordrivesconventionsthatcyclesEarth’scrust,leadingtomelting,crystallization,weathering,anddeformationoflargerockformations,includinggenerationofoceanseaflooratridges,submergenceofoceanseafloorattrenches,mountainbuilding,andactivevolcanicchains.
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ClarificationStatement:
• Theemphasisisonlarge-scalecyclingresultingfromplatetectonics.
NGSSAlignment
Science/EngineeringPractice(SP) DisciplinaryCoreIdea(DCI) CrossCuttingConcepts(CCC)
AnalyzingandInterpretingDataAnalyzingdatain3–5buildsonK–2experiencesandprogressestointroducingquantitativeapproachestocollectingdataandconductingmultipletrialsofqualitativeobservations.Whenpossibleandfeasible,digitaltoolsshouldbeused.Analyzeandinterpretdatatomakesenseofphenomenausinglogicalreasoning.(4-ESS2-2)
ESS2.B:PlateTectonicsandLarge-ScaleSystemInteractions Thelocationsofmountainranges,deepoceantrenches,oceanfloorstructures,earthquakes,andvolcanoesoccurinpatterns.Mostearthquakesandvolcanoesoccurinbandsthatareoftenalongtheboundariesbetweencontinentsandoceans.Majormountainchainsforminsidecontinentsorneartheiredges.MapscanhelplocatethedifferentlandandwaterfeaturesareasofEarth.(4-ESS2-2)
Patterns Patternscanbeusedasevidencetosupportanexplanation.(4-ESS1-1),(4-ESS2-2)
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LearningTargets
1. Icanexplainhowplatetectonicscreateearthquakesandmountains.2. Icandiscusshowvolcanoesareformedandtheeffectsoftheireruptionsonland.3. Icanmodelhowearthquakes,mountains,andvolcanoesarecreated.
AssessmentStudentswillcreatea“NaturalDisaster”newsarticlefortheirPlanetEarthNewspaper
WIDALanguageObjectives(DependentontheneedsofyourELLstudents)
TargetedAcademicLanguage/KeyVocabularyTier2:EarthquakeTier3:TectonicPlates,Faultline
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RESOURCESANDMATERIALSQuantity Item Source
4packages Modelingclay/PlayDoh Bin
1 Smallplasticcup Bin
1tablespoon Flour Bin
2tablespoons Bakingsoda Bin
⅓cup Vinegar Bin
14”square TissuePaper Bin
1roll Papertowels(forcleanup) ClassroomTeacher
1perstudent Scissors ClassroomTeacher
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1 Largerectangularplasticbin Bin
1perstudent ScienceJournal ClassroomTeacher
1perstudent Laptop/iPad ClassroomTeacher
Projector ClassroomTeacher
1perstudent Plasticplates Bin
2boxes GrahamCrackers Bin
3-4containers CoolWhip ContactSueBeauchamp
2 PlasticBowls Bin
DailyPlanetEarthNaturalDisasterArticleTemplate CMCWebsite
IzzyandMaggieGeosquadComic Binder(teachertomakecopiesforstudents)
HowtoDrawtheGeosquadInstructions CMCWebsite
**Itemsinboldshouldbereturnedforusenextyear**
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LESSONDETAILSLessonOpening/Activator
Havetheteacherprojectanimageofavolcanoandaskthestudentswhattheyalreadyknowaboutvolcanoesandearthquakes.Explainthattheywillbelearningaboutvolcanoesandearthquakestoday.DuringtheLesson
1. VolcanoSimulationa. Inordertolearnaboutnaturaldisastersandhowtocreateaplantolessentheireffects,weneedtoknowwhat
happensduringnaturaldisasters.Onetypeofnaturaldisasterisavolcaniceruption.Therearemanyvolcanoes,andoneofthemostfamousisMountSt.HelensinWashingtonStatewhichlasteruptedin2008.Today,wearegoingtosimulateavolcanoerupting.TheScienceFellowsorclassroomteachershouldguidethisexperimentinfrontoftheclass.Beforebeginningtheexperiment,havestudentsdrawa“before”diagramofwhatthevolcanolookslike.Oncetheexperimentiscomplete,askthestudentstodrawan“after”diagramofthevolcanoandhavethestudentswriteasentenceortwoaboutwhathappenedduringtheexperiment.[SP:Patterns]
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b. TheScienceFelloworclassroomteacherwillneedtomakeamodelofavolcanooutofmodelingclayandplaceitintheplasticbinthatisprovided.Thebinwillhelppreventamess.Tocreatethevolcano,shapetheclayaroundtheplasticcupintoaconewiththepointasthetop.Themouthofthecupshouldbeatthetopofthevolcano.
c. OncethemodelvolcanoiscompletetheScienceFellowwillneedtopour2tablespoonsofbakingsodaand1tablespoonofflourintothecenterofa4-inchsquarepieceoftissuepaper.Wrapthetissuepaperaroundthebakingsodaandflourandtwistbothends.ItshouldlookaTootsierollwrappedupwhenitisfinished.
d. Placethemixtureinthecupinthevolcanomodel.
e. Tomakethevolcano“erupt,”pourinhalfoftherequiredamountofvinegar(thisisabout⅙ofacup).Makesuretostepbackalittle,sothemixturedoesnotgetinyoureyesoronyourclothes.Whenthefoamingstops,addtheremainingamountofvinegar(about⅙ofacup).
f. Talktothestudentsandaskthemwhathappened.Whenvolcanoeseruptandthelavacoolsdown,itbuildsthemountainup.Askthestudentswhatkindofrocksareformedfromthecoolingmagma.Thestudentsshouldanswerigneousrocksbasedonwhattheylearnedinpreviouslessons.
g. Therearemanyvolcanoesallovertheworld,especiallylocatedintheringoffire.TheringoffireisanareainthePacificOceanwherethereisacontinuousseriesofoceantrenches,volcanoes,andtectonicplatemovements.
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Notonlyaretherevolcaniceruptionsbutalsothereareseveralearthquakesthatoccurhereduetotectonicplatemovement.
2. RingofFireMappingActivity:a. AssigneachstudenttolookupeitheravolcanooramajorearthquakefromtheRingofFireandfinditslocation
onthemapandoneinterestingfactaboutthephenomena.Interestingfactscaninclude:Howmanytimeshasthevolcanoerupted?Whenisthelasttimeiterupted?Howtallisit?Inthecaseofearthquakes,howfarawaywastheearthquakefelt?Theteachermaywanttowritethesepromptsontheboard.TheSmithsonianInstitute’swebsite(https://volcano.si.edu/search_volcano.cfm)isthebestwebsitetogotoforthoseresearchingvolcanoes,butstudentscanalsolookthemupongooglemapstofigureouttheirlocation.
b. Volcanoes:i. Mt.Erebusii. Mt.Taranakiiii. WhiteIslandiv. WestMatav. Mt.Merapivi. Mt.Pinatubovii. Mt.Fujiviii. SarychevPeakix. Makushin
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x. Mt.Edzizaxi. Mt.St.Helensxii. VolcandeFuegoxiii. Sangayxiv. Llaimaxv. Mt.Hudson
c. Earthquakes:i. 1960Valdiviaearthquakeii. 1906SanFranciscoearthquakeiii. 2011Tohokuearthquakeiv. 1999Ambrymearthquakev. 2010Christchurchearthquake
3. Havetheteacherprojectaworldmapatthefrontoftheclassroom(withawhiteboardorchalkboardbehindtheprojectionifpossible)andaskthestudentstocomeupandpointtothelocationoftheirearthquake/volcano(ifpossiblehavethemmakeadotontheboardofwheretheirearthquake/volcanoislocated).Oncethedotshavebeenmadeontheboard,askthestudentsifthecollectionofvolcanoesandearthquakesformsanyparticularshape.Ifstudentsarehavingahardtimevisualizingtheshape,theteachershouldguidethemtotheconclusionthatthecollectionofdotsshouldformaring,whichiscalledtheRingofFire.
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FunFact:Theringoffirehas452volcanoesandincludes75%ofalloftheworld’svolcanoes,aswellasmostoftheworld’searthquakes!
a. Askthestudentstothinkaboutwhysomanyvolcanoesandearthquakesareclusteredalongthisring.Havethestudentsdoathink-pair-share.Youmayaskprobingquestionstoguidetheirthinking:WhatdoallthespotsalongtheRingofFirehaveincommon?Whymightearthquakesandvolcanoesoccurinsimilarplaces?
b. Afterthestudentshaveofferedtheirideas,havethestudentsreadthecomicaboutplatesubductionwithIzzyandMaggieandengageinadiscussionaboutwhattheylearnedfromthecomic.
4. GrahamCrackerPlateTectonics/EarthquakeActivity:Explaintothestudentsthattheearth’ssurfaceismadeupoflayersandthecrustoftheEarthismadeupoftectonicplates.Astheplatesmoveandcollidewitheachothertheycancausemountainstoformorearthquakestooccur.Handoutthreegrahamcrackerstoeachstudentaswellasaplatewithcoolwhip.Studentsshouldbreakallthegrahamcrackersinhalfinordertoconducttheirexplorations.TellthestudentstheywillbeusingthegrahamcrackerstolearnabouthowdifferentboundariescanaffecttheEarthindifferentways.
5. EarthquakeCreation:Explaintostudentsthatanearthquakeoccurswhentwotectonicplatesgrindpasteachother.Havethestudentstaketwocrackerhalvesandgentlyslidetheiredgesagainstoneanother.Askthestudentstopayattentiontohowthecrackersfeelandthesoundstheymake.Havethestudentsdothisafewtimes.Explainthatearthquakesarecausedwhentheplatescollideandscratchtogether.Asthepressurebetweentheplatesbuilds,the
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platesslipreleasingenergythatwefeelasanearthquake.
6. MountainCreation:Explaintostudentsthatamountainiscreatedwhentwoplatesmovetowardseachother.Whentwoplatesmovetowardeachothertheycancollideandformmountains.Askthestudentstaketwocrackerhalvesandtodiponeendofeachgrahamcrackerinwater,theadultscancarryaroundabowlofwatersothestudentscandiptheircrackersfromtheirseat.Havestudentsplacethecrackerswiththesoggysidesfacingeachotherandaskthemtogentlypushthecrackerstogether.Thecrackersshouldfoldontopofeachother,formingmountains.
7. VolcanoCreation:Explaintostudentsthatavolcanoiscreatedwhenadenseroceanicplateisthrustunderalessdensecontinentalplate.Astheoceanicplatebreaksaway,hotmagmaoozesupandhardenscreatingvolcanicmountains.Studentswilldemonstratethecreationofvolcanoesusingagrahamcracker(brokeninhalf)andaplatewithdollopofcoolwhip.Thestudentsshouldrestthetwohalvesofthegrahamcrackerontopofthecoolwhipandslideonehalfovertheother.Astheyapplypressure,partofonecrackershouldbreakoffandthecoolwhip(themagma)belowthecrackershouldcomeupontothesurface,formingthevolcanoes.
AssessmentStudentswillcreatea“NaturalDisaster”newsarticlefortheirPlanetEarthNewspaper
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Lesson7:ProtectingAgainstNaturalDisasters
LESSONBACKGROUND
ThislessontiestogethereverythingstudentshavebeenlearningaboutdifferentEarthprocesses.ScienceContentBackgroundNaturaldisastersareanyEarthprocessesthatharmanddestroylivingcreaturesandthethingstheyneedtosurvive.Naturaldisasterscanhappenveryslowly,suchasmajordroughts,orveryquickly,suchasearthquakes.Thefirstpriorityindealingwithnaturaldisastersistofindoutwhetherwecanpreventthemfromhappening.Thekeytopreventingdisastersistofigureoutwhatmakesthemhappen.Forexample,floodsoccurwhenthegroundcannotabsorbenoughwater.Wecansometimespreventthegroundfrombeingoverloadedwithwaterbygrowingplantsorsettingupraincatchers.Wecan’tpreventallnaturaldisasters,soit’susefultobeabletofigureoutwhennaturaldisastersaremostlikelytohappen,sothatwecanstartmovingpeopleandvaluableobjectsoutofharmswaywhilewestillhaveenoughtime.Ofcourse,noonecanactuallypredictnaturaldisasters;justlikeaweatherforecast,thebestwecandoisfigureoutwhenthereisagoodchancethatanaturaldisasterwillhappen.Lastly,therearecaseswherewecan’tpreventorpredictnaturaldisastersormightnotbeabletomoveeveryoneandeverythingtosafety.Inthatcase,wecaneitherredirectthedisaster,containit,orwithstandit.OverviewoftheLessonInthislesson,studentswilllearnaboutnaturaldisasters.Theywillthinkaboutpotentialwaystoprotectthemselvesagainstnaturaldisastersorwaystolessentheeffectsbyexperimentingwithvolcanoes,earthquakes,andfloods.FortheDailyPlanet
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Earthnewspaperportfolioprojectstudentswillbecreatinga“HowtoSurvivea[naturaldisaster]”guideandcomic.FocusandSpiralStandardsFocusStandard:4-ESS3-2.Evaluatedifferentsolutionstoreducetheimpactsofanaturaleventsuchasanearthquake,blizzard,orfloodonhumans.*ClarificationStatement:
• Examplesofsolutionscouldincludeanearthquake-resistantbuildingoraconstructedwetlandtomitigateflooding.SpiralStandard:3-ESS3-1.Evaluatethemeritofadesignsolutionthatreducestheimpactsofaweather-relatedhazard.ClarificationStatement:
• Examplesofdesignsolutionstoaweather-relatedhazardcouldincludeabarriertopreventflooding,awind-resistantroofandalightningrod.
SpiralStandard:7.MS-ESS3-2.Obtainandcommunicateinformationonhowdatafrompastgeologiceventsareanalyzedforpatternsandusedtoforecastthelocationandlikelihoodoffuturecatastrophicevents.ClarificationStatements:
• Geologiceventsincludeearthquakes,volcaniceruptions,floods,andlandslides.• Examplesofdatatypicallyanalyzedcanincludethelocations,magnitudes,andfrequenciesofnaturalhazards.
StateAssessmentBoundary:• Activeanalysisofdataorforecastingisnotexpectedinstateassessment.
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Science/EngineeringPractice(SP) DisciplinaryCoreIdea(DCI) CrossCuttingConcepts(CCC)
ConstructingExplanationsandDesigningSolutions
Constructingexplanationsanddesigningsolutionsin3–5buildsonK–2experiencesandprogressestotheuseofevidenceinconstructingexplanationsthatspecifyvariablesthatdescribeandpredictphenomenaandindesigningmultiplesolutionstodesignproblems.
● Identifytheevidencethatsupportsparticularpointsinanexplanation.(4-ESS1-1)
● Generateandcomparemultiplesolutionstoaproblembasedonhowwelltheymeetthecriteriaandconstraintsofthedesignsolution.(4-ESS3-2)
ESS3.B:NaturalHazardsAvarietyofhazardsresultfromnaturalprocesses(e.g.,earthquakes,tsunamis,volcaniceruptions).Humanscannoteliminatethehazardsbutcantakestepstoreducetheirimpacts.(4-ESS3-2)(Note:ThisDisciplinaryCoreIdeacanalsobefoundin3.WC.)ETS1.B:DesigningSolutionstoEngineeringProblemsTestingasolutioninvolvesinvestigatinghowwellitperformsunderarangeoflikelyconditions.(secondaryto4-ESS3-2)
InfluenceofEngineering,Technology,andScienceonSociety
andtheNaturalWorldEngineersimproveexistingtechnologiesordevelopnewonestoincreasetheirbenefits,todecreaseknownrisks,andtomeetsocietaldemands.(4-ESS3-2)
LearningTargetsIcandiscussthreetypesofnaturaldisastersincludingvolcaniceruptions,earthquakes,andfloods.Icandiscusstheimpactsofnaturaldisastersandhowtoprotectagainstorlessentheeffectsofthesenaturaldisasters.
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AssessmentCreatea“HowtoSurvivea[naturaldisaster]”articleforPlanetEarthNewspaper.Eachstudentwillchooseonenaturaldisaster(flood,volcano,orearthquake)towriteabout.WIDALanguageObjectives(DependentontheneedsofyourELLstudents)TargetedAcademicLanguage/KeyVocabulary
Tier2:Flood,Redirect,Contain,Withstand,BarrierTier3:Prevention,Extinction
RESOURCESANDMATERIALSQuantity Item Source
1perstudent “SafeHouses”Article(2pages) Binder
4packages Modelingclay/PlayDoh Bin
1roll Papertowels(forcleanup) ClassroomTeacher
1perstudent Scissors ClassroomTeacher
1 Largebinorbucket Bin
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1perstudent Sciencejournal ClassroomTeacher
1 FloodsinNorthAdamsPowerPoint CMCWebsite
1 DinosaurExtinctionPowerpoint CMCWebsite
1perstudent Laptop/iPad ClassroomTeacher
Projector ClassroomTeacher
1container Legos Bin
6 AluminumPans Bin
12boxes JelloMix Bin
30perstudent Minimarshmallows Bin
30perstudent Toothpicks Bin
2boxes Popsiclesticks Bin
Asneeded Buildingblocks ClassroomTeacher
Asneeded Tape ClassroomTeacher
1roll String Bin
2boxes Plasticspoons Bin
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1pergroup Paperplate Bin
1pergroup BrassFastener Bin
1pergroup Paperclip Bin
2pergroup Cups Bin
Asneeded Glue ClassroomTeacher
1perstudent GeosquadFloodComic Binder
1perstudent BlankComicTemplates CMCWebsite
1perstudent DailyPlanetEarthHowtoSurviveaNaturalDisasterArticleTemplate CMCWebsite
GeosquadFloodVideo CMCWebsite**Itemsinboldshouldbereturnedforusenextyear**
LESSONDETAILSLessonOpening/ActivatorShowstudentstheGeoSquadFloodVideo.Afterthevideo,explaintostudentsthatEarthprocessescanharmanddamagelife,includingpeopleandthestructurestheybuild,arecallednaturaldisasters.AskstudentstothinkabouttheEarthprocessesthey’velearnedaboutthisunit,andwhetheranyofthemcouldbeconsiderednaturaldisasters.Asstudentstosharetheirandcreatealistontheboard.
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DuringtheLesson
1. Sharewiththestudentsthattherearethreemainwaystoprotectagainstanaturaldisaster:redirectingthedanger,containingit,orwithstandingit.Dividetheboardintothreesections,onelabeled“Redirect”,one“Contain”andone“Withstand”.Theteachershouldgooverthevocabularywords(redirect,contain,withstand)withthestudentsbyfirstaskingthemtothinkoftheirowndefinitionsandsharethemwiththeclass.Herearedefinitionsforthewords:
a. Redirect:tochangeorguideanobjectorforcetoanotherarea.b. Contain:toholdasubstanceorobjectc. Withstand:toholdoutagainst,resist,orendure
2. Floods:ExplainthatNorthAdamshasahistoryoffloods,projecttheFloodsinNorthAdamsPowerPointontheboard.a. BuildingaTown:Buildasmalltownandthensimulateaflood.Havethestudentscometothefronttableofthe
classroom.Usingsoilorclay,createabaseforthetowninalargebinorbucket.Ifthereisenoughsoil,buildamountaininthecornerofthebintorepresentMountGreylock.Havepairsofstudentseachcreateasmallbuilding,person,orplanttoputinthetownusingLegos.Oncethetownisassembled,getagallonotsoofwaterandpouritintothebin.Pourthewaterstartingatthetopofthemountain.
b. Askthestudentstotalkdescribewhattheysee.Besuretointroducetheconceptoffloodingandexplainthatiswhattheyarewatchinghappennow.
c. Askstudentstothink-pair-shareideasforhowtopreventfloods.Asthestudentsshareouttheirideas,havetheclassorganizetheideasbasedonwhethertheirplanswouldinvolveredirection,containment,orwithstanding.
2. “SafeHouses”:HandouttheNationalGeographicarticle“SafeHouses”byChrisCarroll.Callonastudenttoreadthetitleandintroductoryparagraph.Explainthatthisarticlewillbeaboutearthquake-proofbuildingsandhomes.Callonadifferentstudenttoreadeachparagraph,pausingbetweeneachtosummarizeconceptsanddefinevocabulary.Atthe
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endofthearticle,askstudentswhattypeofpreventionmethodwasmentionedinthearticle.Theanswershouldbewithstanding.[SP8:obtaininginformation]
***Thislessoncanbebrokenupatthispointiftherearetimelimitations***
3. DisasterPreparednessGame:Thisactivityisadaptedfrom:https://www.teachengineering.org/activities/view/cub_natdis_lesson03_activity1
a. Thisactivitywillneedtobepreparedadayinadvance.Theteacherwillhavetomakejellotofill6aluminumpansthedaybefore.Inthislesson,theclasswillbesplitupintosmallgroupsof3-4students.Sinceclasssizeschange,theteachermayhavetoincreaseordecreasethenumberofaluminumpans.Foreachaluminumpanfullofjello,theteacherwillhavetoalsomakeahousebeforehand.Tocreatethesehouses,theteachershould
connect12toothpickswith8marshmallowstomakeacubeshapedhouse.Pleaseseetheimagebelowforanexample.b. Forthisactivity,tellthestudentsthattheywillbeliketheGeoSquadbecausetheywillsavetheirtownfromnaturaldisasters.Thestudentswillsavethetownbyusingthetoolsfromtheirtoolboxes.Tellthestudentsthatthetoothpick-marshmallowhouseinthealuminumpanwillrepresentallthebuildingsinthetown.c. Beforebeginningtheactivity,dividethestudentsintogroupsandgiveeachgroupapaperplate,abrassfastener,andapapercliptocreatetheirspinners.Forthetoolbox(itemsthestudentscanuseinthisactivity),studentswillbegivenabasketfullofmaterialssuchaspopsiclesticks,toothpicks,plasticspoons,buildingblocks,marshmallows,string,tape,
cardboard,etc.Itisagoodideatolayoutanassortmentofitemsontablesaroundtheroomsothateachgrouphastheirownmaterialstoworkwith.Theteachercanaddadditionalitemsfromtheclassroomifthey’dliketo.
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Eachgroupwillalsobegiventwoplasticcups.Thefirstcupwillbefilledwithwaterandbelabeledasfloodwaters.Theothercupwillbefilledwithglueandbelabeledaslava.Finally,eachgroupwillbegivenatrayofjellowithahouserestingontopofthejello.
d. Tobegintheactivity,theteachershouldaskthestudentstonamethenaturaldisasterstheylearnedaboutinthis
unit.(Theanswershouldbefloods,volcanoeruptions,andearthquakes).Theteachershouldwritethesedisastersonthewhiteboard.Then,theteachershouldtellthestudentstodrawlinesontheirpaperplatestodividetheirspinnersinto3equalsections(triangularshaped).Onesectionshouldsayfloods,thenextshouldsayvolcaniceruptionsandthelastshouldsayearthquakes.Then,thestudentsshouldinsertthebrassfastenerinthemiddleofthepaperplate.Next,thestudentsshouldputoneendofthepapercliparoundthebrassfastener.Finally,thestudentsshouldfoldbacktheendsoftheirbrassfastenertoensureitstaysattachedtothepaperplate.Lookatthepicturebelowforanexampleofwhatthespinnershouldlooklike.
1. Toplaythegame,thestudentsshouldspinthespinnertolandonanaturaldisaster.
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2. Oncestudentslandonanaturaldisaster,theymustdecidewhethertoredirect,contain,orwithstandthisnaturaldisaster,usingthetoolsfromtheirtoolbox.Theteachershouldtellthestudentstorefertothewhiteboardwithexamplesofpreventionmethodsandthearticletheyreadiftheyneedhelp.
3. Thestudentsshouldcreatetheirsolutionsandthentestitoutbyexecutingthenaturaldisaster.Belowisabriefdescriptionofwhattheactivitywilllooklike:
a. Forfloods,therearemanyoptionsforstudents.Theycanusetheplasticspoonstodigfloodchutes(redirecttheflood)orreservoirs(containthefloods).Theycanalsobuildleveesorothertypesofbarrierswithpopsiclesticksorothermaterialstoredirectthefloodwaters.Then,thestudentswillpourthecupofwatertotestwhetherornottheirhousewillbeflooded.
b. Forvolcaniceruptions,thestudentscanusetheplasticspoonstodigchannelstoredirectthelava.Theycanalsobuildtrenchestocontainthelava.Then,studentswilltestwhetherornottheirhouseisburneddownbypouringtheliquidglue(itrepresentslava)ontheiraluminumtray.
c. Forearthquakes,thestudentsshouldusethematerialsfromthetoolboxtoreinforcetheirhouse.Then,thestudentsshouldtestthehouse’ssturdinessbyshakingthetrayofjello.Theinstabilityofthejellomimicsthemovementofthelandduringearthquakes.
d. Aftereachdisaster,thestudentsshouldwriteaboutitintheirsciencejournals.i. Typeofdisaster(flood,volcanoeruption,orearthquake):ii. Preventionmethod(redirect,contain,orwithstand):iii. Descriptionofpreventionmethod(materialsusedandhowtheybuiltit):iv. Didthesolutionwork(yesorno)?v. Waystoimprovetheirsolution:
e. Thestudentsshouldcontinuespinningthespinneruntiltheycompleteall3disasters.
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LessonClosing1. Askstudentstobrainstormideasabouttheextinctionofthedinosaurs.ThenprojecttheDinosaurExtinction
PowerPointontheboard,allowingstudentvolunteerstoreadeachslideoutloud.2. Thenaskstudentstochooseatheoryfromthepowerpointthatresonateswiththem.Creategroupsbasedonwhatthe
studentschooseandgivethemipadstofurtherresearchthetheorytheychoose(youshouldhavefourgroups).Instructthestudentstolookforfactsabouttheirtheory,encouragethemtousethelinksprovidedonthepowerpoint.
3. Onceallthestudentshavefinishedtheirresearch(thisshouldtakenomorethan10-20minutes),tellthestudentstheyaregoingtohaveadebate.Ifpossible,thedebateshouldtakeplaceoutdoors.Pickastudentvolunteerstandinfrontoftheclassandgiveonereasontheothersshouldbelievetheirtheory.Then,pickastudentvolunteerfromadifferentgrouptorespond.Allowthedebatetocarryonwitheachgroupmakingastatementandallowtheothergroupstorespond.
AssessmentForthisassessment,thestudentswillhavetwooptions.Thestudentscaneitherwritea“HowtoSurvive[anaturaldisaster]”articlefortheir“DailyPlanetEarth”Newspaperandmakeacomic,orjustmakeacomicstrip.Eachstudentwillchooseonenaturaldisaster(flood,volcano,orearthquake)towriteabout.Thearticle“SafeHouses”isalsoagreatresourceforideas.Note:Comictemplatesshouldbeprintedbeforehand.Therewillbethreedifferenttemplatesavailable.Pleaseprintoutenoughcopiesofeachtemplate.Tellstudentsthattodaytheywillbecomicstripwritersandexplainthatcomicbooksaremadeupofcomicstrips.Theywillbewritingashortscenedepictinganaturaldisasterandhowtopreventit.Studentscanworkindependentlyorinpairs.Thecomicstripmustcontain:
• Atleastonecharacterthatwillleadthereadersthroughtheplot.
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• Oneofthefollowingnaturaldisasters,andanexplanationofthedisasterthatdemonstratesthestudents’understanding:➢ Earthquake➢ Volcano➢ Floods
• Onewaytopreventthedisasterormitigatedamagetothesurroundingarea
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CurriculumEmbeddedPerformanceAssessmentStandard(s)CoveredbythisAssessment:[2016]4-ESS1-1.Useevidencefromagivenlandscapethatincludessimplelandformsandrocklayerstosupportaclaimabouttheroleoferosionordepositionintheformationofthelandscapeoverlongperiodsoftime.[ClarificationStatements:Examplesofevidenceandclaimscouldincluderocklayerswithshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromdepositiononlandtodepositioninwaterovertime;andacanyonwithrocklayersinthewallsandariverinthebottom,indicatingthatarivererodedtherockovertime.Examplesofsimplelandformscanincludevalleys,hills,mountains,plains,andcanyons.Focusshouldbeonrelativetime.][StateAssessmentBoundary:Specificdetailsofthemechanismsofrockformationorspecificrockformationsandlayersarenotexpectedinstateassessment.]
[2016]4-ESS2-2.AnalyzeandinterpretmapsofEarth’smountainranges,deepoceantrenches,volcanoes,andearthquakeepicenterstodescribepatternsofthesefeaturesandtheirlocationsrelativetoboundariesbetweencontinentsandoceans.StudentLearningTargets
1. Identifywhataphysicalmapisandwhatitconsistsof.2. Readscientificmapsofmountainranges,trenches,activevolcanoes,andearthquakes.(Topographicalmapsnotrequired.)3. Designandtestanerosionpreventionsolution.4. Readscientificmapsofmountainranges,trenches,activevolcanoes,andearthquakes,climateandweather.
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RESOURCESANDMATERIALSQuantity Item Source
3(1pergroup) GeographicmapofMt.Greylock Bin
3(1pergroup) Rectangularclearplasticcontainer Bin
15cups(5cupspergroup)
Topsoil Bin
Asneeded Rocks(smalltomediuminsize) ClassroomTeacher
Asneeded Straws(cutdownthemiddle) Bin
Asneeded Popsiclesticks Bin
1pergroup Cleanketchupbottle Bin
Asneeded Water(tofillketchupbottleswith) ClassroomTeacher
1perstudent Sciencejournal ClassroomTeacher
**Itemsinboldshouldbereturnedforusenextyear**
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Assessment
● DesignanerosionpreventionsystemforasitethatispronetowatererosiononMt.Greylock.Usedifferentbarrierssuchastrees,rocks,anddrainagepipestocreateasituationthatpreventstheleastamountofsoilfromwashingaway.
● Groupsshouldcomeupwithanoralpresentationwhichtouchesonthefollowingquestions:Whydidyoubuildyour
erosionpreventionsystemthisway?Diditworkwell?Procedure:ExplaintostudentsthattheyaregoingtobuildanerosionsystemtoprotectapartofMountGreylockthatcouldbeimpactedbywatererosion.Letthestudentsknowthatthepeopleinthesurroundingtownscannotletthesoilfromthemountainwashdownontotheirhousesoit’suptothemtoplanawaytopreventitfromhappening.
1. Reviewerosionandwatererosionandhowitaffectsalandscape.FeelfreetoreferencetheexperimentdoneinLesson
3.Talkabouthowdifferentthings,suchastreesandrockspreventsoillossaswellashowwatertravelsandcanbefunneled(drainage).
2. Setupthreeworkstationscoveredwithnewspapertomakeforaneasycleanup.Pilesoiltoformaslopeinsideeach
clearplasticcontainer.Theslopewillbedifferentdependingonthecontainerbutshouldbesteepenoughtopromotewaterflow.Oneachdesklayasmallpileofrocks,strawscutdownthemiddle,andpopsiclesticks.
3. HandoutageographicmapofMt.Greylockandhavestudentsreviewthem.Thestudentsshouldpositiontheirmodels
accordingtothemap’sdepictionofthemountainsite.
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4. Describehowweusemodelstoimitatewhatmighthappenonalargerscale.Explaintothestudentsthatwewillpourwateratthetopofthemountaintosimulaterainfall.Theirjobwillbetoworktogetheringroupstoplacerocks,trees(popsiclesticks),anddrainagepipes(straws)onMt.Greylocktopreventsoilerosion.Givestudents15-30minutestodesigntheirerosionpreventionsystemandthencallfortheirattention.
5. Astheyfinishdesigningtheirsystems,gatherallthestudentstocomeovertooneofthegroupsmodels.Havestudents
explainhowtheirlayoutmaysucceedorfailandgetallthestudentstomakeapredictionwhatwillhappen.Pourwaterslowlyonthetopofthemodelfor5secondsandnoticehowmuchsoilwastakenaway.Repeatthisprocessfortheothergroupsmodels
6. Havestudentswriteaparagraphabouthowitemplacementaffectederosionprevention,aswellashowdifferentitems
workedbetterthanothers.AskthestudentstodescribethreewayshowerosionmighthaveaffectedMt.Greylockovertime.
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5EInstructionalModelBackgroundThisinstructionalmodelexistsasasetofphasesforscienceinstructionthatstartswithstudents’priorknowledgeinordertoreconstructanewknowledgewithdeeperunderstanding.TheEngagementphaseisfirst,inwhichteachersandstudentsbegintomulloverquestions,priorknowledgeandunderstanding,andpotentialfrustrationstheymighthavewithatopic.Thisphaseismeanttobeinformal–thisisthestartofthelesson.ThesecondstepinvolvesExploringphenomena,whichactsasanintroductiontothelargerconceptsthatengagesstudentsinahands-onapproach.Afterexploration,Explanationofscientificconceptsbegins.Tofurtherstudentunderstanding,Elaborationisnext,inwhichstudentsarepresentedwithevenmorechallengingactivitiesandproblems.FollowingthelearningprocesscomesEvaluation,asdeemednecessarybylearninggoalsanddefinedachievements.Themodelisbasedonscientificresearchabouthowchildrenlearnandismeanttobefollowedchronologically,althoughsomestepsmayberepeated.
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ScienceTalkandOracyinT2LUnits Sciencetalkismuchmorethantalkingaboutscience.Inlinewiththescienceandengineeringpractices,studentsareexpectedtomakeaclaimthatcanbesupportedbyscientificevidence.TheMASTEStandards(andtheNGSS)valuetheimportanceofengaginginanargumentfromevidence.NGSSdefineshowthispracticetakesformintherealworld:“Inscience,reasoningandargumentareessentialforidentifyingthestrengthsandweaknessesofalineofreasoningandforfindingthebestexplanationforanaturalphenomenon.Scientistsmustdefendtheirexplanations,formulateevidencebasedonasolidfoundationofdata,examinetheirownunderstandinginlightoftheevidenceandcommentsofferedbyothers,andcollaboratewithpeersinsearchingforthebestexplanationforthephenomenonbeinginvestigated.”Studentsareaskedtoparticipateinarticulateandsensibleconversationsinwhichtheyareabletocommunicatetheirideaseffectively,listentoothers tounderstand, clarify andelaborate ideas, and reflectupon theirunderstanding.These formsof talk canbedevelopedusingscaffoldssuchastheA/BTalkprotocol(below)andstrategies forclassdiscussions(fromtheTalkSciencePrimer, linkbelow).Oracy isdevelopedinthephysical,linguistic,cognitive,andsocial-emotionalrealms;eachoftheserealmscanbeexpandeduponovertimeinorderto develop a thoughtful speaker. Being able to display appropriate body language, use proper tone and grammar, be thoughtful andconsideratethinkers,andallowspaceforotherthoughtsandopinionsareallimportantfacetsoforacytoworkonandthroughwithstudents.Incorporatingtheappropriatescaffoldingisanimportantaspectoffosteringtheseskills.Techniquesforteachingeffectivesciencetalkoftenincludemodeling,discussionguidelines,sentence-starters,andgeneratingroles,whilegraduallyputtingmoreresponsibilityonstudentstoowntheirthinkingandlearning.Partofcreatingasafeschoolenvironmentforstudentsisallowingthemaspacethatiscomfortableenoughforthemtoexpressideasandaskquestions,whilebeingvalidatedfortheirthoughtsandquestions;studentsshouldbefeelcomfortableandconfidentwhenspeakingandlisteningforunderstanding.Effectivetalkisanimportantpartofbeinganactive,intelligentmemberofacommunityandsociety.Successfuldevelopmentinoracyisimportantforfutureemployabilityandgeneralwell-beingofadults.Thefollowingresourcesshouldbehelpfulexamplesofhowtoemployeffectiveuseofprogressiveoracyandsciencetalkinyourclassrooms.
● OracyintheClassroom:https://www.edutopia.org/practice/oracy-classroom-strategies-effective-talk● ScienceTalkPrimer:https://inquiryproject.terc.edu/shared/pd/TalkScience_Primer.pdf
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● A/BTalkProtocolAdaptedfromhttps://ambitiousscienceteaching.org/ab-partner-talk-protocol/
1.ShareyourideasPartnerA● Ithink_______happenedbecause…● Evidencethatsupportsmyideais…● Theactivitywedidwith_______helpsme
knowmoreabout_______because…● OnethingI’mwonderingaboutis…
2.ListentoUnderstandPartnerB● Iheardyousay_______.Whatmakesyouthinkthat?
● Iheardyousay_______.Whatif_______?● Canyouexplainthepartabout_______again?● Whatdoyoumeanwhenyousay_______?
3.ClarifyandelaboratePartnerA
Answerpartner’squestionsoraskforclarificationinordertounderstandaquestion.
4.Repeatsteps2&3untilallquestionsareanswered
5.Switchrolesandrepeatsteps1-4
6.Reflectonyourunderstandinginwriting● Myideaabout_______changedwhenmypartnersaid
_______.● Iwilladd_______tomyideaabout_______because…● Istillhavequestionsabout…● Imaybeabletoanswermyquestion(s)ifIcould
investigate_______.
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UnitActivityPlanner
Activity LearningTargets ScienceConnectionto
PhenomenaMAStandards
Lesson1Activity1:OnlineMapsActivity2:DailyPlanetEarthNewspaper
• Icanidentifyaphysicalmapanditscomponents.
• Icanreadmapsthatdepictmountainranges,trenches,activevolcanoes,andearthquakes.
Studentswillusemapstonotepatternsintheearth’ssurface.Specifically,howearthquakeproneareashavevolcanoesandmountains.Mapswillhelpstudentslearnthatlandformsarenotrandomlyformed.
FocusStandard:[2016]4-ESS2-2.AnalyzeandinterpretmapsofEarth’smountainranges,deepoceantrenches,volcanoes,andearthquakeepicenterstodescribepatternsofthesefeaturesandtheirlocationsrelativetoboundariesbetweencontinentsandoceans.
Lesson2Activity1:PhysicalPropertiesofMineralsActivity2:MohsHardnessScaleActivity3:MineralObservationStationsActivity4:Mineral
• Icanperformappropriateteststodeterminethehardness,color,luster,cleavage,andstreakofdifferentminerals.
• Icannotedifferencesbetweenrocksandminerals.
• Icanusepreviously
Studentswilllearnabouttheformationofrockswhichmakeuptheearth’ssurface.Forinstance,fromvolcaniceruptions,igneousrocksform.Inaddition,thepressureandheatfromtheshiftingoftectonicplatesduring
FocusStandard:(4-ESS1-1)Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.ClarificationStatement:Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachange
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IdentificationActivity5:TheMysteryRockExperimentActivity6:MineralAd
recordeddatatoidentifydifferentminerals.
earthquakesformmetamorphicrocks.Otherrockssuchassedimentaryrockstakeawhiletoform,sinceittakesyearsoferosiontocreatethelayersofparticleswhichcomposetheserocks.
fromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.][AssessmentBoundary:Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrockformationsandlayers.Assessmentislimitedtorelativetime.]
Lesson3Activity1:WeatheringandErosionActivity2:ErosionandAbrasionStationsActivity3:WashingAwayLandformsActivity4:BerkshireLandformsActivity5:Mt.GreylockArticle
• Icanobserveanddescribeexamplesofweatheringthroughfrostwedging,abrasionandtreerootwedging.
• Icanobserveanddescribeexamplesoferosionthroughwind,water,andice.
• Icanexplainthedifferencebetween“weathering”and“erosion”.
Studentswilllearnhownaturalphenomenonsuchasthemeltingofglaciers,wind,floods,andothertypesoferosionandweatheringcreatelandformssuchassanddunesandvalleys.
(4-ESS1-1)Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.[ClarificationStatement:Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughthe
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rock.]4-ESS2-1.Makeobservationsandcollectdatatoprovideevidencethatrocks,soils,andsedimentsarebrokenintosmallerpiecesthroughmechanicalweatheringandmovedaroundthrougherosion.[ClarificationStatements:Mechanicalweatheringprocessescanincludefrostwedging,abrasion,andtreerootwedging.Erosioncanincludemovementbyblowingwind,flowingwater,andmovingice.][StateAssessmentBoundary:Chemicalprocessesarenotexpectedinstateassessment.]
Lesson4Activity1:SoilExplorationActivity2:IMOWAChartActivity3:SoilDiscovery
• Icanexplainhowsoilisformedthroughdecompositionandweathering.
• Icanillustratetheconnectionbetweensoilformation(e.g.ratiosoforganicmattertominerals)anditscolorandtexture.
Inthislesson,studentswilllearntheeffectsofweatheringanderosion.Specifically,howweatheringanderosionbreakdownrocksintosmallerparticlestocreatesoil.Studentswillalsolearnhownatural
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Activity4:SoilRecipeActivity5:SoilDrainageTest
• Icanidentifyanddescribethedifferencesbetweensoil,loam,andclay.
processessuchasthedecompositionofplantandanimalmattercreatesoil.Inthisway,studentswilllearnhowsoiltypeplaysahugefactorinnaturaldisasters.Soilsuchassandcannotholdalotofwater,soitismoresusceptibletoflooding.
Lesson5Activity1:MakeyourownfossilActivity2:FossilizationGameActivity3:FossilMapActivity4:Writeaboutyourfossil
• Icanmakewriteastoryaboutmyfossilandthelifethatitlived.
• Icanexplainthedifferencesbetweentypesoffossils.
Studentswilllearnaboutwhathappenedtotheremainsofthedinosaurs.Thedinosaursbecamefossilsafteryearsoferosion.Asaresult,theywereburiedinthesedimentaryrockwhichmakesuptheearth’scrust.Inthisway,studentslearnhowfossilsareembeddedintheearth’ssurface.
(4-ESS1-1)Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.[ClarificationStatement:Examplesofevidencefrompatternscouldincluderocklayerswithmarineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicating
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thatovertimearivercutthroughtherock.][AssessmentBoundary:Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrockformationsandlayers.Assessmentislimitedtorelativetime.]
Lesson6Activity1:VolcanoSimulationActivity2:RingofFireMappingActivity3:GrahamCrackerPlateTectonics/Earthquake
• Icanexplainhowplatetectonicscreateearthquakesandmountains.
• Icandiscusshowvolcanoesareformedandtheeffectsoftheireruptionsonland.
• Icanmodelhowearthquakes,mountains,andvolcanoesarecreated.
Inthislesson,studentswilllearnhowplatemovementscausenaturaldisasterssuchasearthquakesandvolcaniceruptions.Thetectonicplatesalsoformlandformssuchasmountains.
4-ESS2-2.(4-ESS2-2)AnalyzeandinterpretdatafrommapstodescribepatternsofEarth’sfeatures.[ClarificationStatement:MapscanincludetopographicmapsofEarth’slandandoceanfloor,aswellasmapsofthelocationsofmountains,continentalboundaries,volcanoes,andearthquakes.
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Lesson7Activity1:FloodsActivity2:“SafeHouses”Activity3:DisasterPreparednessGame
• Icandiscussthreetypesofnaturaldisastersincludingvolcaniceruptions,earthquakes,andfloods.
• Icandiscusstheimpactsofnaturaldisastersandhowtoprotectagainstorlessentheeffectsofthesenaturaldisasters.
Studentswilllearnaboutthedamagescausedbynaturaldisastersandpreventionmethods.
[2016]4-ESS3-2.Evaluatedifferentsolutionstoreducetheimpactsofanaturaleventsuchasanearthquake,blizzard,orfloodonhumans.*[ClarificationStatement:Examplesofsolutionscouldincludeanearthquake-resistantbuildingoraconstructedwetlandtomitigateflooding.]
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NGSSAlignmentTableStudents who demonstrate understanding can: (4-ESS1-1)Identifyevidencefrompatternsinrockformationsandfossilsinrocklayerstosupportanexplanationforchangesinalandscapeovertime.[ClarificationStatement:Examplesofevidencefrompatternscouldincluderocklayerswithma-rineshellfossilsaboverocklayerswithplantfossilsandnoshells,indicatingachangefromlandtowaterovertime;and,acanyonwithdifferentrocklayersinthewallsandariverinthebottom,indicatingthatovertimearivercutthroughtherock.][AssessmentBoundary:Assessmentdoesnotincludespecificknowledgeofthemechanismofrockformationormemorizationofspecificrockfor-mationsandlayers.Assessmentislimitedtorelativetime.] (4-ESS2-1)Makeobservationsand/ormeasurementstoprovideevidenceoftheeffectsofweatheringortherateoferosionbywater,ice,wind,orvegetation.[ClarificationStatement:Examplesofvariablestotestcouldincludeangleofslopeinthedownhillmovementofwater,amountofvegetation,speedofwind,relativerateofdeposition,cyclesoffreezingandthawingofwater,cyclesofheatingandcooling,andvolumeofwaterflow.][AssessmentBoundary:Assessmentislimitedtoasingleformofweatheringorerosion.] (4-ESS2-2)AnalyzeandinterpretdatafrommapstodescribepatternsofEarth’sfeatures.[ClarificationStatement:MapscanincludetopographicmapsofEarth’slandandoceanfloor,aswellasmapsofthelocationsofmountains,continentalboundaries,volca-noes,andearthquakes.] (4-ESS3-2)GenerateandcomparemultiplesolutionstoreducetheimpactsofnaturalEarthprocessesonhumans.*[Clarifica-tionStatement:Examplesofsolutionscouldincludedesigninganearthquakeresistantbuildingandimprovingmonitoringofvolcanicactivity.][AssessmentBoundary:Assessmentislimitedtoearthquakes,floods,tsunamis,andvolcaniceruptions.]
The performance expectations above were developed using the following elements from the NRC document A Framework for K-12 Science Education:
ScienceandEngineeringPracticesPlanningandCarryingOutInvestiga-
tions
DisciplinaryCoreIdeasESS1.C:TheHistoryofPlanetEarth
Local,regional,andglobalpatternsofrockformationsrevealchangesovertimedue
CrosscuttingConceptsPatterns:Patternscanbeusedasevi-dencetosupportanexplanation.(4-
ESS1-1),(4-ESS2-2)
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Planningandcarryingoutinvestiga-tionstoanswerquestionsortestsolu-tionstoproblemsin3–5buildsonK–2experiencesandprogressestoincludeinvestigationsthatcontrolvariables
andprovideevidencetosupportexpla-nationsordesignsolutions.
Makeobservationsand/ormeasure-mentstoproducedatatoserveasthebasisforevidenceforanexplanationof
aphenomenon.(4-ESS2-1)AnalyzingandInterpretingData
Analyzingdatain3–5buildsonK–2ex-periencesandprogressestointroduc-ingquantitativeapproachestocollect-ingdataandconductingmultipletrialsofqualitativeobservations.Whenpos-sibleandfeasible,digitaltoolsshould
beused.Analyzeandinterpretdatatomakesenseofphenomenausinglogicalrea-
soning.(4-ESS2-2)ConstructingExplanationsandDe-
signingSolutions
toEarthforces,suchasearthquakes.Thepresenceandlocationofcertainfossil
typesindicatetheorderinwhichrocklay-erswereformed.(4-ESS1-1)
ESS2.A:EarthMaterialsandSystemsRainfallhelpstoshapethelandandaffectsthetypesoflivingthingsfoundinaregion.Water,ice,wind,livingorganisms,andgravitybreakrocks,soils,andsedimentsintosmallerparticlesandmovethem
around.(4-ESS2-1)ESS2.B:PlateTectonicsandLarge-
ScaleSystemInteractionsThelocationsofmountainranges,deepoceantrenches,oceanfloorstructures,earthquakes,andvolcanoesoccurinpat-terns.Mostearthquakesandvolcanoesoc-
curinbandsthatareoftenalongtheboundariesbetweencontinentsand
oceans.Majormountainchainsformin-sidecontinentsorneartheiredges.Mapscanhelplocatethedifferentlandandwa-terfeaturesareasofEarth.(4-ESS2-2)
ESS2.E:BiogeologyLivingthingsaffectthephysicalcharac-teristicsoftheirregions.(4-ESS2-1)
CauseandEffectCauseandeffectrelationshipsarerou-tinelyidentified,tested,andusedtoex-plainchange.(4-ESS2-1),(4-ESS3-2)-----------------------------------------------ConnectionstoEngineering,Tech-nology,andApplicationsofScienceInfluenceofEngineering,Technology,andScienceonSocietyandtheNatural
WorldEngineersimproveexistingtechnolo-giesordevelopnewonestoincreasetheirbenefits,todecreaseknownrisks,andtomeetsocietaldemands.(4-ESS3-
2)ConnectionstoNatureofScience
ScientificKnowledgeAssumesanOrderandConsistencyinNaturalSystems
Scienceassumesconsistentpatternsinnaturalsystems.(4-ESS1-1)
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Constructingexplanationsanddesign-ingsolutionsin3–5buildsonK–2ex-periencesandprogressestotheuseofevidenceinconstructingexplanationsthatspecifyvariablesthatdescribeandpredictphenomenaandindesigningmultiplesolutionstodesignproblems.Identifytheevidencethatsupportspar-ticularpointsinanexplanation.(4-
ESS1-1)Generateandcomparemultiplesolu-tionstoaproblembasedonhowwelltheymeetthecriteriaandconstraintsofthedesignsolution.(4-ESS3-2)
ESS3.B:NaturalHazardsAvarietyofhazardsresultfromnaturalprocesses(e.g.,earthquakes,tsunamis,
volcaniceruptions).Humanscannotelimi-natethehazardsbutcantakestepstore-ducetheirimpacts.(4-ESS3-2)(Note:ThisDisciplinaryCoreIdeacanalsobefoundin
3.WC.)ETS1.B:DesigningSolutionstoEngi-
neeringProblemsTestingasolutioninvolvesinvestigatinghowwellitperformsunderarangeof
likelyconditions.(secondaryto4-ESS3-2
ConnectionstootherDCIsinthirdgrade:4.ETS1.C(4-ESS3-2)
ArticulationofDCIsacrossgrade-levels::K.ETS1.A(4-ESS3-2);2.ESS1.C(4-ESS1-1),(4-ESS2-1);2.ESS2.A(4-ESS2-1);2.ESS2.B(4-ESS2-2);2.ESS2.C(4-ESS2-2);2.ETS1.B(4-ESS3-2);2.ETS1.C(4-ESS3-2);3.LS4.A(4-ESS1-1);5.ESS2.A(4-ESS2-1);5.ESS2.C(4-ESS2-2);MS.LS4.A(4-ESS1-1);MS.ESS1.C(4-ESS1-1),(4-ESS2-2);MS.ESS2.A(4-ESS1-1),(4-ESS2-2),(4-ESS3-2);MS.ESS2.B(4-ESS1-1),(4-ESS2-2);MS.ESS3.B(4-ESS3-2);MS.ETS1.B(4-ESS3-2)
CommonCoreStateStandardsConnections:ELA/Literacy—
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RI.4.1Refertodetailsandexamplesinatextwhenexplainingwhatthetextsaysexplicitlyandwhendrawinginferencesfromthetext.(4-ESS3-2)RI.4.7Interpretinformationpresentedvisually,orally,orquantitatively(e.g.,incharts,graphs,diagrams,timelines,animations,orinteractiveelementsonWebpages)andexplainhowtheinformationcontributestoanunderstandingofthetextinwhichitappears.(4-ESS2-2)RI.4.9Integrateinformationfromtwotextsonthesametopicinordertowriteorspeakaboutthesubjectknowledgeably.(4-ESS3-2)W.4.7Conductshortresearchprojectsthatbuildknowledgethroughinvestigationofdifferentaspectsofatopic.(4-ESS1-1),(4-ESS2-1)W.4.8Recallrelevantinformationfromexperiencesorgatherrelevantinformationfromprintanddigitalsources;takenotesandcate-gorizeinformationandprovidealistofsources.(4-ESS1-1),(4-ESS2-1)W.4.9Drawevidencefromliteraryorinformationaltextstosupportanalysis,reflection,andresearch.(4-ESS1-1)Mathematics–MP.2Reasonabstractlyandquantitatively.(4-ESS1-1),(4-ESS2-1),(4-ESS3-2)MP.4Modelwithmathematics.(4-ESS1-1),(4-ESS2-1),(4-ESS3-2)MP.5Useappropriatetoolsstrategically.(4-ESS2-1)4.MD.A.1Knowrelativesizesofmeasurementunitswithinonesystemofunitsincludingkm,m,cm;kg,g;lb,oz.;l,ml;hr,min,sec.Withinasinglesystemofmeasurement,expressmeasurementsinalargerunitintermsofasmallerunit.Recordmeasurementequiv-alentsinatwo-columntable.(4-ESS1-1),(4-ESS2-1)4.MD.A.2Usethefouroperationstosolvewordproblemsinvolvingdistances,intervalsoftime,liquidvolumes,massesofobjects,andmoney,includingproblemsinvolvingsimplefractionsordecimals,andproblemsthatrequireexpressingmeasurementsgiveninalargerunitintermsofasmallerunit.Representmeasurementquantitiesusingdiagramssuchasnumberlinediagramsthatfeatureameasurementscale.(4-ESS2-1),(4-ESS2-2)
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ListofUnitResourcesLesson1
Quantity Item Source
1map Politicalmap Bin
1map Roadmap Bin
1map Attractionmap Bin
1map Topographicalmap Bin
1map Physicalmap Bin
1map Weathermap Bin
1perstudent Laptop/iPad ClassroomTeacher
1perstudent MapFeaturesWorksheet CMCWebsite
1perstudent GoogleEarthWorksheet CMCWebsite
1perstudent BlankTemplateofMassachusetts CMCWebsiteLesson2
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Quantity Item Source
1perstudent HandLens Bin
5Whiteand5Blackplates(1pergroup)
Streakplates Bin
5pergroup Penny Bin
5pergroup Nail Bin
1boxperclass MineralKit-Includes15mineralsamples Bin
1perpair/group Limestonesample Bin
1perpair/group Quartzsample Bin
1perstudent ScienceJournal ClassroomTeacher
RockCleavageVideohttps://www.youtube.com/watch?v=zAOTfSWjw0Q&list=PLsAWD8mKKE95eF864ryLNK8SXJfJ-EsWh&index=1
CMCWebsite
1piece ChartPaper ClassroomTeacher
1 “HowtoDescribeLuster”Board Bin
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1perstudent RocksandMineralsComparisonChart Binder
1perstudent MineralObservationChart Binder
1perstudent MCASquestion Binder
1 MineralsandRocksPowerPoint CMCWebsite
1perstudent GeoSquadComic Binder
1perstudent DailyPlanetEarthMineralAdvertisementTemplate CMCWebsiteLesson3
Quantity Item Source
1perclassroom Computer+projector ClassroomTeacher
1perclassroom Weathering&ErosionPowerPoint CMCWebsite
1perclassroom ActivityStationSetup(Rock&Roll,andSweptAway:HandsonNaturep.253-254(eachofthesestationsrequirenumerousmaterials,besuretousecornmealforthesweptawaystationratherthanrice)
Binder
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What’sStrongEnoughtoMakeaCanyon?https://tinyurl.com/ybzlhu2g) CMCWebsite
1pergroup Stickytack Bin
2(1perSplashstation;1perSweptstation)
Bakingpan Bin
1perSplashstation Tablespoon Bin
2perstudent 3oz.Dixiecups Bin
1perstudent Spoon Bin
1pergroup Paperplateandplasticplate Bin
Asneeded Cinnamon Bin
Asneeded Salt Bin
1pergroup 2binderclips Bin
1pergroup 2plasticcups Bin
1pergroup 1plasticcondimentcontainer Bin
1pergroup Ruler ClassroomTeacher
1setperclassroom LaminatedImagesofBerkshireLandforms Bin
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Asneeded Water ClassroomTeacher
2perRockstation Clean,sealableplasticcontainer Bin
3handfuls(2perRockstation;1perSweptstation)
Stones Bin
1perclassroom Smallbagofcornmeal Bin
1handfulperSweptstation Blocksofwood Bin
1perstudent Straws Bin
1perstudent “PreparingforDisaster”reading Binder
1perstudent “WatchforSteadyRocks”reading Binder
1perstudent PairedTextQuestionsWorksheet Binder
10 Smallplasticdinosaurs BinLesson4
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Quantity Item Source
2cupsperstudent
SoilfromDecayingMatter Bin
1perstudent Woodenskewers Bin
Asneededtocoverdesks
Newspaper ClassroomTeacher
1perstudent HandLens Bin
2perclass Sieve Bin
1perstudent ScienceJournal ClassroomTeacher
1piece Chartpaper ClassroomTeacher
15(3pergroup)
SodaBottles(funnel,planter,screen) Bin
15cups(3cupspergroup)
Sand Bin
15cups(3cupspergroup)
Pottingsoil Bin
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15cups(3cupspergroup)
Clay Bin
Asneeded Water ClassroomTeacher
5(1pergroup)
Measuringcup Bin
1 SpencerPowerPoint CMCWebsite
1 DailyPlanetEarthSoilRecipeTemplate CMCWebsite
1 IMOWAChart BinderLesson5
Quantity Items Source
6(twoofeachtype) Differenttypesoffossils Bin
1bag WholeWheatFlour Bin
2containers Salt Bin
1 Measuringcup(thatcanmeasureatleast1cup)
Bin
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Variousitemstopressintosaltdoughtomakefossils
ClassroomTeacher/Outdoors
1perstudent FossilHandout Binder(teachertomakecopies)
FossilPowerPoint CMCWebsite
DailyPlanetEarthFossilArticleTemplate CMCWebsite
Laptops/iPads ClassroomTeacherLesson6
Quantity Item Source
4packages Modelingclay/PlayDoh Bin
1 Smallplasticcup Bin
1tablespoon Flour Bin
2tablespoons Bakingsoda Bin
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⅓cup Vinegar Bin
14”square TissuePaper Bin
1roll Papertowels(forcleanup) ClassroomTeacher
1perstudent Scissors ClassroomTeacher
1 Largerectangularplasticbin Bin
1perstudent ScienceJournal ClassroomTeacher
1perstudent Laptop/iPad ClassroomTeacher
Projector ClassroomTeacher
1perstudent Plasticplates Bin
2boxes GrahamCrackers Bin
3-4containers CoolWhip ContactSueBeauchamp
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2 PlasticBowls Bin
DailyPlanetEarthNaturalDisasterArticleTemplate CMCWebsite
IzzyandMaggieGeosquadComic Binder(teachertomakecopiesforstudents)
HowtoDrawtheGeosquadInstructions CMCWebsite
Lesson7
Quantity Item Source
1perstudent “SafeHouses”Article(2pages) Binder
4packages Modelingclay/PlayDoh Bin
1roll Papertowels(forcleanup) ClassroomTeacher
1perstudent Scissors ClassroomTeacher
1 Largebinorbucket Bin
1perstudent Sciencejournal ClassroomTeacher
1 FloodsinNorthAdamsPowerPoint CMCWebsite
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1 DinosaurExtinctionPowerpoint CMCWebsite
1perstudent Laptop/iPad ClassroomTeacher
Projector ClassroomTeacher
1container Legos Bin
6 AluminumPans Bin
12boxes JelloMix Bin
30perstudent Minimarshmallows Bin
30perstudent Toothpicks Bin
2boxes Popsiclesticks Bin
Asneeded Buildingblocks ClassroomTeacher
Asneeded Tape ClassroomTeacher
1roll String Bin
2boxes Plasticspoons Bin
1pergroup Paperplate Bin
1pergroup BrassFastener Bin
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1pergroup Paperclip Bin
2pergroup Cups Bin
Asneeded Glue ClassroomTeacher
1perstudent GeosquadFloodComic Binder
1perstudent BlankComicTemplates CMCWebsite
1perstudent DailyPlanetEarthHowtoSurviveaNaturalDisasterArticleTemplate CMCWebsite
GeosquadFloodVideo CMCWebsite
CEPA
Quantity Item Source
3(1pergroup) GeographicmapofMt.Greylock Bin
3(1pergroup) Rectangularclearplasticcontainer Bin
15cups(5cupspergroup)
Topsoil Bin
Asneeded Rocks(smalltomediuminsize) ClassroomTeacher
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Asneeded Straws(cutdownthemiddle) Bin
Asneeded Popsiclesticks Bin
1pergroup Cleanketchupbottle Bin
Asneeded Water(tofillketchupbottleswith) ClassroomTeacher
1perstudent Sciencejournal ClassroomTeacher