transformboundaryplatesslide pasteachothermantlethickestlayer ofearthfaultbreak inearth'scrustconvergentboundarymovestogetherlavamoltenrock aboveEarth’ssurfacemountainsform hereconvergentboundaryriftvalleysform heredivergentboundarymagmamoltenrock underEarth’ssurfacesecondaryventmagmacan reachthe surfaceinother areasdivergentboundarymovesapartPangeasupercontinentinnercoresolid ironandnickelsecondaryconelava buildsup here inthe shapeof a conehurricanelarge swirlingstorm thatforms overoceanspyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanocratercircularbasin ordepressionmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacevolcanicbombslargeprojectilesthrownthroughthe airsubductionwhen oneplate slidesunderanother10010 x10ashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionmatteranything thattakes upspace andhas masscrustouter,thinnestlayer ofearthmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crusttransformboundaryplatesslide pasteachothermantlethickestlayer ofearthfaultbreak inearth'scrustconvergentboundarymovestogetherlavamoltenrock aboveEarth’ssurfacemountainsform hereconvergentboundaryriftvalleysform heredivergentboundarymagmamoltenrock underEarth’ssurfacesecondaryventmagmacan reachthe surfaceinother areasdivergentboundarymovesapartPangeasupercontinentinnercoresolid ironandnickelsecondaryconelava buildsup here inthe shapeof a conehurricanelarge swirlingstorm thatforms overoceanspyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanocratercircularbasin ordepressionmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacevolcanicbombslargeprojectilesthrownthroughthe airsubductionwhen oneplate slidesunderanother10010 x10ashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionmatteranything thattakes upspace andhas masscrustouter,thinnestlayer ofearthmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crust

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