crustouter,thinnestlayer ofearthmountainsform hereconvergentboundaryvolcanicbombslargeprojectilesthrownthroughthe airhurricanelarge swirlingstorm thatforms overoceansashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionconvergentboundarymovestogetherPangeasupercontinentpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomantlethickestlayer ofearth10010 x10subductionwhen oneplate slidesunderanotherdivergentboundarymovesapartmatteranything thattakes upspace andhas massmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustcratercircularbasin ordepressionsecondaryventmagmacan reachthe surfaceinother areasriftvalleysform heredivergentboundarytransformboundaryplatesslide pasteachotherinnercoresolid ironandnickelmagmamoltenrock underEarth’ssurfacefaultbreak inearth'scrustlavamoltenrock aboveEarth’ssurfacemainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesecondaryconelava buildsup here inthe shapeof a conecrustouter,thinnestlayer ofearthmountainsform hereconvergentboundaryvolcanicbombslargeprojectilesthrownthroughthe airhurricanelarge swirlingstorm thatforms overoceansashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionconvergentboundarymovestogetherPangeasupercontinentpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomantlethickestlayer ofearth10010 x10subductionwhen oneplate slidesunderanotherdivergentboundarymovesapartmatteranything thattakes upspace andhas massmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustcratercircularbasin ordepressionsecondaryventmagmacan reachthe surfaceinother areasriftvalleysform heredivergentboundarytransformboundaryplatesslide pasteachotherinnercoresolid ironandnickelmagmamoltenrock underEarth’ssurfacefaultbreak inearth'scrustlavamoltenrock aboveEarth’ssurfacemainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesecondaryconelava buildsup here inthe shapeof a cone

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