mountainsform hereconvergentboundaryconvergentboundarymovestogethermagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustsecondaryconelava buildsup here inthe shapeof a conemagmamoltenrock underEarth’ssurfacelavamoltenrock aboveEarth’ssurfacehurricanelarge swirlingstorm thatforms overoceansvolcanicbombslargeprojectilesthrownthroughthe aircrustouter,thinnestlayer ofearthsubductionwhen oneplate slidesunderanotherpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanodivergentboundarymovesapartsecondaryventmagmacan reachthe surfaceinother areasmatteranything thattakes upspace andhas massriftvalleysform heredivergentboundaryfaultbreak inearth'scrustinnercoresolid ironandnickel10010 x10ashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptiontransformboundaryplatesslide pasteachotherPangeasupercontinentcratercircularbasin ordepressionmantlethickestlayer ofearthmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacemountainsform hereconvergentboundaryconvergentboundarymovestogethermagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustsecondaryconelava buildsup here inthe shapeof a conemagmamoltenrock underEarth’ssurfacelavamoltenrock aboveEarth’ssurfacehurricanelarge swirlingstorm thatforms overoceansvolcanicbombslargeprojectilesthrownthroughthe aircrustouter,thinnestlayer ofearthsubductionwhen oneplate slidesunderanotherpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanodivergentboundarymovesapartsecondaryventmagmacan reachthe surfaceinother areasmatteranything thattakes upspace andhas massriftvalleysform heredivergentboundaryfaultbreak inearth'scrustinnercoresolid ironandnickel10010 x10ashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptiontransformboundaryplatesslide pasteachotherPangeasupercontinentcratercircularbasin ordepressionmantlethickestlayer ofearthmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surface

Plate tectonics - 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. convergent boundary
    mountains form here
  2. moves together
    convergent boundary
  3. large underground pool of molten rock sitting underneath Earth’s crust
    magma chamber
  4. lava builds up here in the shape of a cone
    secondary cone
  5. molten rock under Earth’s surface
    magma
  6. molten rock above Earth’s surface
    lava
  7. large swirling storm that forms over oceans
    hurricane
  8. large projectiles thrown through the air
    volcanic bombs
  9. outer, thinnest layer of earth
    crust
  10. when one plate slides under another
    subduction
  11. fast moving current of hot gas and rock that moves away from a volcano
    pyroclastic flow
  12. moves apart
    divergent boundary
  13. magma can reach the surface in other areas
    secondary vent
  14. anything that takes up space and has mass
    matter
  15. divergent boundary
    rift valleys form here
  16. break in earth's crust
    fault
  17. solid iron and nickel
    inner core
  18. 10 x 10
    100
  19. small pieces of pulverized rock, minerals, and volcanic glass created during eruption
    ash cloud
  20. plates slide past each other
    transform boundary
  21. supercontinent
    Pangea
  22. circular basin or depression
    crater
  23. thickest layer of earth
    mantle
  24. the weak point in Earth’s crust where hot magma rises from the magma chamber and reaches the surface
    main vent