mid-oceanridgelittoralzonethe spacebetweenhigh andlow tidesedimentationsediments arebroken down,transported,and depositedin a nee placecurrentcontinuousmovement ofwater due todensity orwindelniñoiceerosionglaciers pick upand transportsediments asthey move overland.corehotsphere ofdenseelementsrockyshorethis shoreis resistanttoweatheringdivergentboundarytransformboundarywinderosionwind picksup sedimentand carries itto a newlocationlaniñadeltaform at themouth of ariver where itmeets thesradiurnaloccuringdailyseastackphysicalweatheringtemperaturechangescreatecracks inrocksseacavecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.springtidesun andmoon alignto create alarger tidalrangewatererosiona river picksup sedimentsand carriesthem to theoceanestuaryform inshelteredareas wherefresh and saltwater meetsurfacecurrentsthesecurrentsare drivenby windorganicweatheringlichen attachto balsalticrock andbreak downparticles.muddyshorethis shoreis shallowwith noslopeseaarchheadlandtidalrangedifferencebetweenhigh tideand low tidesemi-diurnaloccuringtwicedailymantlehot, semi-solid rockunderneaththe crustdeepcurrentsthese currentsare driven bydifferences indensity andsalinitychemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffsandyshorethis shoreis formedby erosionlithosphereoutermostlayer ofthe earthgravityerosiona piece of acliff's edgefalls intowater belowpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorseastumptideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeconvergentboundarymid-oceanridgelittoralzonethe spacebetweenhigh andlow tidesedimentationsediments arebroken down,transported,and depositedin a nee placecurrentcontinuousmovement ofwater due todensity orwindelniñoiceerosionglaciers pick upand transportsediments asthey move overland.corehotsphere ofdenseelementsrockyshorethis shoreis resistanttoweatheringdivergentboundarytransformboundarywinderosionwind picksup sedimentand carries itto a newlocationlaniñadeltaform at themouth of ariver where itmeets thesradiurnaloccuringdailyseastackphysicalweatheringtemperaturechangescreatecracks inrocksseacavecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.springtidesun andmoon alignto create alarger tidalrangewatererosiona river picksup sedimentsand carriesthem to theoceanestuaryform inshelteredareas wherefresh and saltwater meetsurfacecurrentsthesecurrentsare drivenby windorganicweatheringlichen attachto balsalticrock andbreak downparticles.muddyshorethis shoreis shallowwith noslopeseaarchheadlandtidalrangedifferencebetweenhigh tideand low tidesemi-diurnaloccuringtwicedailymantlehot, semi-solid rockunderneaththe crustdeepcurrentsthese currentsare driven bydifferences indensity andsalinitychemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffsandyshorethis shoreis formedby erosionlithosphereoutermostlayer ofthe earthgravityerosiona piece of acliff's edgefalls intowater belowpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorseastumptideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pullneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeconvergentboundary

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. mid-ocean ridge
  2. the space between high and low tide
    littoral zone
  3. sediments are broken down, transported, and deposited in a nee place
    sedimentation
  4. continuous movement of water due to density or wind
    current

  5. el niño
  6. glaciers pick up and transport sediments as they move over land.
    ice erosion
  7. hot sphere of dense elements
    core
  8. this shore is resistant to weathering
    rocky shore

  9. divergent boundary

  10. transform boundary
  11. wind picks up sediment and carries it to a new location
    wind erosion

  12. la niña
  13. form at the mouth of a river where it meets the sra
    delta
  14. occuring daily
    diurnal

  15. sea stack
  16. temperature changes create cracks in rocks
    physical weathering

  17. sea cave
  18. earth's rotation causes currents to move clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
    coriolis effect
  19. sun and moon align to create a larger tidal range
    spring tide
  20. a river picks up sediments and carries them to the ocean
    water erosion
  21. form in sheltered areas where fresh and salt water meet
    estuary
  22. these currents are driven by wind
    surface currents
  23. lichen attach to balsaltic rock and break down particles.
    organic weathering
  24. this shore is shallow with no slope
    muddy shore

  25. sea arch

  26. headland
  27. difference between high tide and low tide
    tidal range
  28. occuring twice daily
    semi-diurnal
  29. hot, semi-solid rock underneath the crust
    mantle
  30. these currents are driven by differences in density and salinity
    deep currents
  31. new rock exposed to precipitation dissolves ions and transports it to the ocean as runoff
    chemical weathering
  32. this shore is formed by erosion
    sandy shore
  33. outermost layer of the earth
    lithosphere
  34. a piece of a cliff's edge falls into water below
    gravity erosion
  35. patterns of polarity and reversed polarity on the sea floor
    paleomagnetic strips

  36. sea stump
  37. regular rise and fall of the ocean surface due to the sun and moon's gravitacional pull
    tide
  38. sun and moon form a right angle with the earth to create a smaller tidal range
    neap tide

  39. convergent boundary