springtidesun andmoon alignto create alarger tidalrangeseastackrockyshorethis shoreis resistanttoweatheringcorehotsphere ofdenseelementsgravityerosiona piece of acliff's edgefalls intowater belowdeepcurrentsthese currentsare driven bydifferences indensity andsalinitymantlehot, semi-solid rockunderneaththe crustconvergentboundarylithosphereoutermostlayer ofthe earthtideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullestuaryform inshelteredareas wherefresh and saltwater meetdivergentboundarysurfacecurrentsthesecurrentsare drivenby windlaniñasedimentationsediments arebroken down,transported,and depositedin a nee placediurnaloccuringdailydeltaform at themouth of ariver where itmeets thesrawatererosiona river picksup sedimentsand carriesthem to theoceanwinderosionwind picksup sedimentand carries itto a newlocationcorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.organicweatheringlichen attachto balsalticrock andbreak downparticles.littoralzonethe spacebetweenhigh andlow tidemid-oceanridgecurrentcontinuousmovement ofwater due todensity orwindsemi-diurnaloccuringtwicedailyelniñoneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeiceerosionglaciers pick upand transportsediments asthey move overland.muddyshorethis shoreis shallowwith noslopetransformboundarytidalrangedifferencebetweenhigh tideand low tideseacavephysicalweatheringtemperaturechangescreatecracks inrockschemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffseastumppaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorheadlandsandyshorethis shoreis formedby erosionseaarchspringtidesun andmoon alignto create alarger tidalrangeseastackrockyshorethis shoreis resistanttoweatheringcorehotsphere ofdenseelementsgravityerosiona piece of acliff's edgefalls intowater belowdeepcurrentsthese currentsare driven bydifferences indensity andsalinitymantlehot, semi-solid rockunderneaththe crustconvergentboundarylithosphereoutermostlayer ofthe earthtideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullestuaryform inshelteredareas wherefresh and saltwater meetdivergentboundarysurfacecurrentsthesecurrentsare drivenby windlaniñasedimentationsediments arebroken down,transported,and depositedin a nee placediurnaloccuringdailydeltaform at themouth of ariver where itmeets thesrawatererosiona river picksup sedimentsand carriesthem to theoceanwinderosionwind picksup sedimentand carries itto a newlocationcorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.organicweatheringlichen attachto balsalticrock andbreak downparticles.littoralzonethe spacebetweenhigh andlow tidemid-oceanridgecurrentcontinuousmovement ofwater due todensity orwindsemi-diurnaloccuringtwicedailyelniñoneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeiceerosionglaciers pick upand transportsediments asthey move overland.muddyshorethis shoreis shallowwith noslopetransformboundarytidalrangedifferencebetweenhigh tideand low tideseacavephysicalweatheringtemperaturechangescreatecracks inrockschemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffseastumppaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorheadlandsandyshorethis shoreis formedby erosionseaarch

AICE Marine Bingo! by Emily Sanchez - Call List

(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.


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