divergentboundaryestuaryform inshelteredareas wherefresh and saltwater meetmuddyshorethis shoreis shallowwith noslopecorehotsphere ofdenseelementstransformboundaryphysicalweatheringtemperaturechangescreatecracks inrocksheadlandsemi-diurnaloccuringtwicedailyseastacksandyshorethis shoreis formedby erosionpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorseastumpmantlehot, semi-solid rockunderneaththe crustlittoralzonethe spacebetweenhigh andlow tidecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.diurnaloccuringdailyseaarchgravityerosiona piece of acliff's edgefalls intowater belowspringtidesun andmoon alignto create alarger tidalrangelithosphereoutermostlayer ofthe earthorganicweatheringlichen attachto balsalticrock andbreak downparticles.tideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pulldeepcurrentsthese currentsare driven bydifferences indensity andsalinitycurrentcontinuousmovement ofwater due todensity orwindrockyshorethis shoreis resistanttoweatheringwatererosiona river picksup sedimentsand carriesthem to theoceanwinderosionwind picksup sedimentand carries itto a newlocationlaniñaneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeiceerosionglaciers pick upand transportsediments asthey move overland.chemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffsedimentationsediments arebroken down,transported,and depositedin a nee placedeltaform at themouth of ariver where itmeets thesraconvergentboundarytidalrangedifferencebetweenhigh tideand low tideelniñomid-oceanridgesurfacecurrentsthesecurrentsare drivenby windseacavedivergentboundaryestuaryform inshelteredareas wherefresh and saltwater meetmuddyshorethis shoreis shallowwith noslopecorehotsphere ofdenseelementstransformboundaryphysicalweatheringtemperaturechangescreatecracks inrocksheadlandsemi-diurnaloccuringtwicedailyseastacksandyshorethis shoreis formedby erosionpaleomagneticstripspatterns ofpolarity andreversedpolarity onthe sea floorseastumpmantlehot, semi-solid rockunderneaththe crustlittoralzonethe spacebetweenhigh andlow tidecorioliseffectearth's rotationcauses currents tomove clockwise inthe northernhemisphere andcounterclockwise inthe southernhemisphere.diurnaloccuringdailyseaarchgravityerosiona piece of acliff's edgefalls intowater belowspringtidesun andmoon alignto create alarger tidalrangelithosphereoutermostlayer ofthe earthorganicweatheringlichen attachto balsalticrock andbreak downparticles.tideregular rise andfall of the oceansurface due tothe sun andmoon'sgravitacional pulldeepcurrentsthese currentsare driven bydifferences indensity andsalinitycurrentcontinuousmovement ofwater due todensity orwindrockyshorethis shoreis resistanttoweatheringwatererosiona river picksup sedimentsand carriesthem to theoceanwinderosionwind picksup sedimentand carries itto a newlocationlaniñaneaptidesun and moonform a rightangle with theearth to createa smaller tidalrangeiceerosionglaciers pick upand transportsediments asthey move overland.chemicalweatheringnew rock exposedto precipitationdissolves ions andtransports it to theocean as runoffsedimentationsediments arebroken down,transported,and depositedin a nee placedeltaform at themouth of ariver where itmeets thesraconvergentboundarytidalrangedifferencebetweenhigh tideand low tideelniñomid-oceanridgesurfacecurrentsthesecurrentsare drivenby windseacave

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. divergent boundary
  2. form in sheltered areas where fresh and salt water meet
    estuary
  3. this shore is shallow with no slope
    muddy shore
  4. hot sphere of dense elements
    core

  5. transform boundary
  6. temperature changes create cracks in rocks
    physical weathering

  7. headland
  8. occuring twice daily
    semi-diurnal

  9. sea stack
  10. this shore is formed by erosion
    sandy shore
  11. patterns of polarity and reversed polarity on the sea floor
    paleomagnetic strips

  12. sea stump
  13. hot, semi-solid rock underneath the crust
    mantle
  14. the space between high and low tide
    littoral zone
  15. earth's rotation causes currents to move clockwise in the northern hemisphere and counterclockwise in the southern hemisphere.
    coriolis effect
  16. occuring daily
    diurnal

  17. sea arch
  18. a piece of a cliff's edge falls into water below
    gravity erosion
  19. sun and moon align to create a larger tidal range
    spring tide
  20. outermost layer of the earth
    lithosphere
  21. lichen attach to balsaltic rock and break down particles.
    organic weathering
  22. regular rise and fall of the ocean surface due to the sun and moon's gravitacional pull
    tide
  23. these currents are driven by differences in density and salinity
    deep currents
  24. continuous movement of water due to density or wind
    current
  25. this shore is resistant to weathering
    rocky shore
  26. a river picks up sediments and carries them to the ocean
    water erosion
  27. wind picks up sediment and carries it to a new location
    wind erosion

  28. la niña
  29. sun and moon form a right angle with the earth to create a smaller tidal range
    neap tide
  30. glaciers pick up and transport sediments as they move over land.
    ice erosion
  31. new rock exposed to precipitation dissolves ions and transports it to the ocean as runoff
    chemical weathering
  32. sediments are broken down, transported, and deposited in a nee place
    sedimentation
  33. form at the mouth of a river where it meets the sra
    delta

  34. convergent boundary
  35. difference between high tide and low tide
    tidal range

  36. el niño

  37. mid-ocean ridge
  38. these currents are driven by wind
    surface currents

  39. sea cave