surfacecurrentsthesecurrentsare drivenby windneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangetideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pulldivergentboundaryseacaveestuaryform inshelteredareas wherefresh and saltwater meetmuddyshorethis shoreis shallowwith noslopeconvergentboundarypaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorwinderosionwind picksup sedimentand carries itto a newlocationheadlandlaniñarockyshorethis shoreis resistanttoweatheringdeepcurrentsthese currentsare driven bydifferences indensity andsalinitytransformboundarydiurnaloccuringdailywatererosiona river picksup sedimentsand carriesthem to theoceandeltaform at themouth of ariver where itmeets thesraseastumpelniñocorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.springtidesun andmoon alignto create alarger tidalrangetidalrangedifferencebetweenhigh tideand low tidegravityerosiona piece of acliff's edgefalls intowater beloworganicweatheringlichen attachto balsalticrock andbreak downparticles.sedimentationsediments arebroken down,transported,and depositedin a nee placecorehotsphere ofdenseelementslithosphereoutermostlayer ofthe earthiceerosionglaciers pick upand transportsediments asthey move overland.seaarchphysicalweatheringtemperaturechangescreatecracks inrockschemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffmid-oceanridgemantlehot, semi-solid rockunderneaththe crustseastacksemi-diurnaloccuringtwicedailycurrentcontinuousmovement ofwater due todensity orwindsandyshorethis shoreis formedby erosionlittoralzonethe spacebetweenhigh andlow tidesurfacecurrentsthesecurrentsare drivenby windneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangetideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pulldivergentboundaryseacaveestuaryform inshelteredareas wherefresh and saltwater meetmuddyshorethis shoreis shallowwith noslopeconvergentboundarypaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorwinderosionwind picksup sedimentand carries itto a newlocationheadlandlaniñarockyshorethis shoreis resistanttoweatheringdeepcurrentsthese currentsare driven bydifferences indensity andsalinitytransformboundarydiurnaloccuringdailywatererosiona river picksup sedimentsand carriesthem to theoceandeltaform at themouth of ariver where itmeets thesraseastumpelniñocorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.springtidesun andmoon alignto create alarger tidalrangetidalrangedifferencebetweenhigh tideand low tidegravityerosiona piece of acliff's edgefalls intowater beloworganicweatheringlichen attachto balsalticrock andbreak downparticles.sedimentationsediments arebroken down,transported,and depositedin a nee placecorehotsphere ofdenseelementslithosphereoutermostlayer ofthe earthiceerosionglaciers pick upand transportsediments asthey move overland.seaarchphysicalweatheringtemperaturechangescreatecracks inrockschemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffmid-oceanridgemantlehot, semi-solid rockunderneaththe crustseastacksemi-diurnaloccuringtwicedailycurrentcontinuousmovement ofwater due todensity orwindsandyshorethis shoreis formedby erosionlittoralzonethe spacebetweenhigh andlow tide

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. these currents are driven by wind
    surface currents
  2. sun and moon form a right angle with the earth to create a smaller tidal range
    neap tide
  3. regular rise and fall of the ocean surface due to the sun and moon's gravitacional pull
    tide

  4. divergent boundary

  5. sea cave
  6. form in sheltered areas where fresh and salt water meet
    estuary
  7. this shore is shallow with no slope
    muddy shore

  8. convergent boundary
  9. patterns of polarity and reversed polarity on the sea floor
    paleomagnetic strips
  10. wind picks up sediment and carries it to a new location
    wind erosion

  11. headland

  12. la niña
  13. this shore is resistant to weathering
    rocky shore
  14. these currents are driven by differences in density and salinity
    deep currents

  15. transform boundary
  16. occuring daily
    diurnal
  17. a river picks up sediments and carries them to the ocean
    water erosion
  18. form at the mouth of a river where it meets the sra
    delta

  19. sea stump

  20. el niño
  21. earth's rotation causes currents to move clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
    coriolis effect
  22. sun and moon align to create a larger tidal range
    spring tide
  23. difference between high tide and low tide
    tidal range
  24. a piece of a cliff's edge falls into water below
    gravity erosion
  25. lichen attach to balsaltic rock and break down particles.
    organic weathering
  26. sediments are broken down, transported, and deposited in a nee place
    sedimentation
  27. hot sphere of dense elements
    core
  28. outermost layer of the earth
    lithosphere
  29. glaciers pick up and transport sediments as they move over land.
    ice erosion

  30. sea arch
  31. temperature changes create cracks in rocks
    physical weathering
  32. new rock exposed to precipitation dissolves ions and transports it to the ocean as runoff
    chemical weathering

  33. mid-ocean ridge
  34. hot, semi-solid rock underneath the crust
    mantle

  35. sea stack
  36. occuring twice daily
    semi-diurnal
  37. continuous movement of water due to density or wind
    current
  38. this shore is formed by erosion
    sandy shore
  39. the space between high and low tide
    littoral zone