crustouter,thinnestlayer ofearthsecondaryconelava buildsup here inthe shapeof a conefaultbreak inearth'scrustconvergentboundarymovestogethervolcanicbombslargeprojectilesthrownthroughthe airhurricanelarge swirlingstorm thatforms overoceanstransformboundaryplatesslide pasteachotherdivergentboundarymovesapartcratercircularbasin ordepressionlavamoltenrock aboveEarth’ssurfacemainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacepyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomountainsform hereconvergentboundarymagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustmagmamoltenrock underEarth’ssurfacematteranything thattakes upspace andhas masssubductionwhen oneplate slidesunderanotherinnercoresolid ironandnickel10010 x10Pangeasupercontinentmantlethickestlayer ofearthsecondaryventmagmacan reachthe surfaceinother areasashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionriftvalleysform heredivergentboundarycrustouter,thinnestlayer ofearthsecondaryconelava buildsup here inthe shapeof a conefaultbreak inearth'scrustconvergentboundarymovestogethervolcanicbombslargeprojectilesthrownthroughthe airhurricanelarge swirlingstorm thatforms overoceanstransformboundaryplatesslide pasteachotherdivergentboundarymovesapartcratercircularbasin ordepressionlavamoltenrock aboveEarth’ssurfacemainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacepyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomountainsform hereconvergentboundarymagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustmagmamoltenrock underEarth’ssurfacematteranything thattakes upspace andhas masssubductionwhen oneplate slidesunderanotherinnercoresolid ironandnickel10010 x10Pangeasupercontinentmantlethickestlayer ofearthsecondaryventmagmacan reachthe surfaceinother areasashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionriftvalleysform heredivergentboundary

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