seacavediurnaloccuringdailysurfacecurrentsthesecurrentsare drivenby windseastumprockyshorethis shoreis resistanttoweatheringsemi-diurnaloccuringtwicedailyneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangemid-oceanridgeelniñomantlehot, semi-solid rockunderneaththe crustcurrentcontinuousmovement ofwater due todensity orwindmuddyshorethis shoreis shallowwith noslopeorganicweatheringlichen attachto balsalticrock andbreak downparticles.divergentboundarysandyshorethis shoreis formedby erosiontransformboundarycorehotsphere ofdenseelementsconvergentboundarychemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runofflaniñaheadlandiceerosionglaciers pick upand transportsediments asthey move overland.deepcurrentsthese currentsare driven bydifferences indensity andsalinityseastacklittoralzonethe spacebetweenhigh andlow tidecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.tideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullwatererosiona river picksup sedimentsand carriesthem to theoceanseaarchestuaryform inshelteredareas wherefresh and saltwater meetdeltaform at themouth of ariver where itmeets thesraphysicalweatheringtemperaturechangescreatecracks inrockswinderosionwind picksup sedimentand carries itto a newlocationsedimentationsediments arebroken down,transported,and depositedin a nee placetidalrangedifferencebetweenhigh tideand low tidegravityerosiona piece of acliff's edgefalls intowater belowpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorspringtidesun andmoon alignto create alarger tidalrangelithosphereoutermostlayer ofthe earthseacavediurnaloccuringdailysurfacecurrentsthesecurrentsare drivenby windseastumprockyshorethis shoreis resistanttoweatheringsemi-diurnaloccuringtwicedailyneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangemid-oceanridgeelniñomantlehot, semi-solid rockunderneaththe crustcurrentcontinuousmovement ofwater due todensity orwindmuddyshorethis shoreis shallowwith noslopeorganicweatheringlichen attachto balsalticrock andbreak downparticles.divergentboundarysandyshorethis shoreis formedby erosiontransformboundarycorehotsphere ofdenseelementsconvergentboundarychemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runofflaniñaheadlandiceerosionglaciers pick upand transportsediments asthey move overland.deepcurrentsthese currentsare driven bydifferences indensity andsalinityseastacklittoralzonethe spacebetweenhigh andlow tidecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.tideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullwatererosiona river picksup sedimentsand carriesthem to theoceanseaarchestuaryform inshelteredareas wherefresh and saltwater meetdeltaform at themouth of ariver where itmeets thesraphysicalweatheringtemperaturechangescreatecracks inrockswinderosionwind picksup sedimentand carries itto a newlocationsedimentationsediments arebroken down,transported,and depositedin a nee placetidalrangedifferencebetweenhigh tideand low tidegravityerosiona piece of acliff's edgefalls intowater belowpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorspringtidesun andmoon alignto create alarger tidalrangelithosphereoutermostlayer ofthe earth

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. sea cave
  2. occuring daily
    diurnal
  3. these currents are driven by wind
    surface currents

  4. sea stump
  5. this shore is resistant to weathering
    rocky shore
  6. occuring twice daily
    semi-diurnal
  7. sun and moon form a right angle with the earth to create a smaller tidal range
    neap tide

  8. mid-ocean ridge

  9. el niño
  10. hot, semi-solid rock underneath the crust
    mantle
  11. continuous movement of water due to density or wind
    current
  12. this shore is shallow with no slope
    muddy shore
  13. lichen attach to balsaltic rock and break down particles.
    organic weathering

  14. divergent boundary
  15. this shore is formed by erosion
    sandy shore

  16. transform boundary
  17. hot sphere of dense elements
    core

  18. convergent boundary
  19. new rock exposed to precipitation dissolves ions and transports it to the ocean as runoff
    chemical weathering

  20. la niña

  21. headland
  22. glaciers pick up and transport sediments as they move over land.
    ice erosion
  23. these currents are driven by differences in density and salinity
    deep currents

  24. sea stack
  25. the space between high and low tide
    littoral zone
  26. earth's rotation causes currents to move clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
    coriolis effect
  27. regular rise and fall of the ocean surface due to the sun and moon's gravitacional pull
    tide
  28. a river picks up sediments and carries them to the ocean
    water erosion

  29. sea arch
  30. form in sheltered areas where fresh and salt water meet
    estuary
  31. form at the mouth of a river where it meets the sra
    delta
  32. temperature changes create cracks in rocks
    physical weathering
  33. wind picks up sediment and carries it to a new location
    wind erosion
  34. sediments are broken down, transported, and deposited in a nee place
    sedimentation
  35. difference between high tide and low tide
    tidal range
  36. a piece of a cliff's edge falls into water below
    gravity erosion
  37. patterns of polarity and reversed polarity on the sea floor
    paleomagnetic strips
  38. sun and moon align to create a larger tidal range
    spring tide
  39. outermost layer of the earth
    lithosphere