semi-diurnaloccuringtwicedailyestuaryform inshelteredareas wherefresh and saltwater meetdiurnaloccuringdailyphysicalweatheringtemperaturechangescreatecracks inrockstideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pulldivergentboundaryseastumpheadlandsedimentationsediments arebroken down,transported,and depositedin a nee placecorehotsphere ofdenseelementswatererosiona river picksup sedimentsand carriesthem to theoceanneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeseaarchiceerosionglaciers pick upand transportsediments asthey move overland.convergentboundarytidalrangedifferencebetweenhigh tideand low tideelniñoseacavemid-oceanridgewinderosionwind picksup sedimentand carries itto a newlocationmantlehot, semi-solid rockunderneaththe crustchemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffseastackgravityerosiona piece of acliff's edgefalls intowater belowcurrentcontinuousmovement ofwater due todensity orwindorganicweatheringlichen attachto balsalticrock andbreak downparticles.muddyshorethis shoreis shallowwith noslopedeltaform at themouth of ariver where itmeets thesralithosphereoutermostlayer ofthe earthtransformboundarylittoralzonethe spacebetweenhigh andlow tidecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.laniñapaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorsurfacecurrentsthesecurrentsare drivenby windrockyshorethis shoreis resistanttoweatheringspringtidesun andmoon alignto create alarger tidalrangesandyshorethis shoreis formedby erosiondeepcurrentsthese currentsare driven bydifferences indensity andsalinitysemi-diurnaloccuringtwicedailyestuaryform inshelteredareas wherefresh and saltwater meetdiurnaloccuringdailyphysicalweatheringtemperaturechangescreatecracks inrockstideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pulldivergentboundaryseastumpheadlandsedimentationsediments arebroken down,transported,and depositedin a nee placecorehotsphere ofdenseelementswatererosiona river picksup sedimentsand carriesthem to theoceanneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeseaarchiceerosionglaciers pick upand transportsediments asthey move overland.convergentboundarytidalrangedifferencebetweenhigh tideand low tideelniñoseacavemid-oceanridgewinderosionwind picksup sedimentand carries itto a newlocationmantlehot, semi-solid rockunderneaththe crustchemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffseastackgravityerosiona piece of acliff's edgefalls intowater belowcurrentcontinuousmovement ofwater due todensity orwindorganicweatheringlichen attachto balsalticrock andbreak downparticles.muddyshorethis shoreis shallowwith noslopedeltaform at themouth of ariver where itmeets thesralithosphereoutermostlayer ofthe earthtransformboundarylittoralzonethe spacebetweenhigh andlow tidecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.laniñapaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorsurfacecurrentsthesecurrentsare drivenby windrockyshorethis shoreis resistanttoweatheringspringtidesun andmoon alignto create alarger tidalrangesandyshorethis shoreis formedby erosiondeepcurrentsthese currentsare driven bydifferences indensity andsalinity

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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  1. occuring twice daily
    semi-diurnal
  2. form in sheltered areas where fresh and salt water meet
    estuary
  3. occuring daily
    diurnal
  4. temperature changes create cracks in rocks
    physical weathering
  5. regular rise and fall of the ocean surface due to the sun and moon's gravitacional pull
    tide

  6. divergent boundary

  7. sea stump

  8. headland
  9. sediments are broken down, transported, and deposited in a nee place
    sedimentation
  10. hot sphere of dense elements
    core
  11. a river picks up sediments and carries them to the ocean
    water erosion
  12. sun and moon form a right angle with the earth to create a smaller tidal range
    neap tide

  13. sea arch
  14. glaciers pick up and transport sediments as they move over land.
    ice erosion

  15. convergent boundary
  16. difference between high tide and low tide
    tidal range

  17. el niño

  18. sea cave

  19. mid-ocean ridge
  20. wind picks up sediment and carries it to a new location
    wind erosion
  21. hot, semi-solid rock underneath the crust
    mantle
  22. new rock exposed to precipitation dissolves ions and transports it to the ocean as runoff
    chemical weathering

  23. sea stack
  24. a piece of a cliff's edge falls into water below
    gravity erosion
  25. continuous movement of water due to density or wind
    current
  26. lichen attach to balsaltic rock and break down particles.
    organic weathering
  27. this shore is shallow with no slope
    muddy shore
  28. form at the mouth of a river where it meets the sra
    delta
  29. outermost layer of the earth
    lithosphere

  30. transform boundary
  31. the space between high and low tide
    littoral zone
  32. earth's rotation causes currents to move clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
    coriolis effect

  33. la niña
  34. patterns of polarity and reversed polarity on the sea floor
    paleomagnetic strips
  35. these currents are driven by wind
    surface currents
  36. this shore is resistant to weathering
    rocky shore
  37. sun and moon align to create a larger tidal range
    spring tide
  38. this shore is formed by erosion
    sandy shore
  39. these currents are driven by differences in density and salinity
    deep currents