volcanicbombslargeprojectilesthrownthroughthe airashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptioninnercoresolid ironandnickelmantlethickestlayer ofearthhurricanelarge swirlingstorm thatforms overoceanslavamoltenrock aboveEarth’ssurfacefaultbreak inearth'scrustsecondaryventmagmacan reachthe surfaceinother areasmountainsform hereconvergentboundarysubductionwhen oneplate slidesunderanothermainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacetransformboundaryplatesslide pasteachotherconvergentboundarymovestogetherpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustsecondaryconelava buildsup here inthe shapeof a conedivergentboundarymovesapartriftvalleysform heredivergentboundarymatteranything thattakes upspace andhas massPangeasupercontinentcratercircularbasin ordepressionmagmamoltenrock underEarth’ssurfacecrustouter,thinnestlayer ofearth10010 x10volcanicbombslargeprojectilesthrownthroughthe airashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptioninnercoresolid ironandnickelmantlethickestlayer ofearthhurricanelarge swirlingstorm thatforms overoceanslavamoltenrock aboveEarth’ssurfacefaultbreak inearth'scrustsecondaryventmagmacan reachthe surfaceinother areasmountainsform hereconvergentboundarysubductionwhen oneplate slidesunderanothermainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacetransformboundaryplatesslide pasteachotherconvergentboundarymovestogetherpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustsecondaryconelava buildsup here inthe shapeof a conedivergentboundarymovesapartriftvalleysform heredivergentboundarymatteranything thattakes upspace andhas massPangeasupercontinentcratercircularbasin ordepressionmagmamoltenrock underEarth’ssurfacecrustouter,thinnestlayer ofearth10010 x10

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