elniñosurfacecurrentsthesecurrentsare drivenby windseacavewatererosiona river picksup sedimentsand carriesthem to theoceanpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorlittoralzonethe spacebetweenhigh andlow tidewinderosionwind picksup sedimentand carries itto a newlocationorganicweatheringlichen attachto balsalticrock andbreak downparticles.currentcontinuousmovement ofwater due todensity orwindtransformboundarylaniñalithosphereoutermostlayer ofthe earthtidalrangedifferencebetweenhigh tideand low tiderockyshorethis shoreis resistanttoweatheringdeltaform at themouth of ariver where itmeets thesraheadlandchemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffestuaryform inshelteredareas wherefresh and saltwater meetconvergentboundarymuddyshorethis shoreis shallowwith noslopemantlehot, semi-solid rockunderneaththe crustphysicalweatheringtemperaturechangescreatecracks inrocksseaarchseastumpcorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.springtidesun andmoon alignto create alarger tidalrangecorehotsphere ofdenseelementsdiurnaloccuringdailysemi-diurnaloccuringtwicedailydivergentboundaryiceerosionglaciers pick upand transportsediments asthey move overland.sandyshorethis shoreis formedby erosiondeepcurrentsthese currentsare driven bydifferences indensity andsalinitymid-oceanridgetideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullseastacksedimentationsediments arebroken down,transported,and depositedin a nee placegravityerosiona piece of acliff's edgefalls intowater belowneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeelniñosurfacecurrentsthesecurrentsare drivenby windseacavewatererosiona river picksup sedimentsand carriesthem to theoceanpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorlittoralzonethe spacebetweenhigh andlow tidewinderosionwind picksup sedimentand carries itto a newlocationorganicweatheringlichen attachto balsalticrock andbreak downparticles.currentcontinuousmovement ofwater due todensity orwindtransformboundarylaniñalithosphereoutermostlayer ofthe earthtidalrangedifferencebetweenhigh tideand low tiderockyshorethis shoreis resistanttoweatheringdeltaform at themouth of ariver where itmeets thesraheadlandchemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffestuaryform inshelteredareas wherefresh and saltwater meetconvergentboundarymuddyshorethis shoreis shallowwith noslopemantlehot, semi-solid rockunderneaththe crustphysicalweatheringtemperaturechangescreatecracks inrocksseaarchseastumpcorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.springtidesun andmoon alignto create alarger tidalrangecorehotsphere ofdenseelementsdiurnaloccuringdailysemi-diurnaloccuringtwicedailydivergentboundaryiceerosionglaciers pick upand transportsediments asthey move overland.sandyshorethis shoreis formedby erosiondeepcurrentsthese currentsare driven bydifferences indensity andsalinitymid-oceanridgetideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullseastacksedimentationsediments arebroken down,transported,and depositedin a nee placegravityerosiona piece of acliff's edgefalls intowater belowneaptidesun and moonform a rightangle with theearth to createa smaller tidalrange

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. el niño
  2. these currents are driven by wind
    surface currents

  3. sea cave
  4. a river picks up sediments and carries them to the ocean
    water erosion
  5. patterns of polarity and reversed polarity on the sea floor
    paleomagnetic strips
  6. the space between high and low tide
    littoral zone
  7. wind picks up sediment and carries it to a new location
    wind erosion
  8. lichen attach to balsaltic rock and break down particles.
    organic weathering
  9. continuous movement of water due to density or wind
    current

  10. transform boundary

  11. la niña
  12. outermost layer of the earth
    lithosphere
  13. difference between high tide and low tide
    tidal range
  14. this shore is resistant to weathering
    rocky shore
  15. form at the mouth of a river where it meets the sra
    delta

  16. headland
  17. new rock exposed to precipitation dissolves ions and transports it to the ocean as runoff
    chemical weathering
  18. form in sheltered areas where fresh and salt water meet
    estuary

  19. convergent boundary
  20. this shore is shallow with no slope
    muddy shore
  21. hot, semi-solid rock underneath the crust
    mantle
  22. temperature changes create cracks in rocks
    physical weathering

  23. sea arch

  24. sea stump
  25. earth's rotation causes currents to move clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
    coriolis effect
  26. sun and moon align to create a larger tidal range
    spring tide
  27. hot sphere of dense elements
    core
  28. occuring daily
    diurnal
  29. occuring twice daily
    semi-diurnal

  30. divergent boundary
  31. glaciers pick up and transport sediments as they move over land.
    ice erosion
  32. this shore is formed by erosion
    sandy shore
  33. these currents are driven by differences in density and salinity
    deep currents

  34. mid-ocean ridge
  35. regular rise and fall of the ocean surface due to the sun and moon's gravitacional pull
    tide

  36. sea stack
  37. sediments are broken down, transported, and deposited in a nee place
    sedimentation
  38. a piece of a cliff's edge falls into water below
    gravity erosion
  39. sun and moon form a right angle with the earth to create a smaller tidal range
    neap tide