magmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustriftvalleysform heredivergentboundarytransformboundaryplatesslide pasteachothercrustouter,thinnestlayer ofearthmountainsform hereconvergentboundarylavamoltenrock aboveEarth’ssurfacecratercircularbasin ordepressionsecondaryventmagmacan reachthe surfaceinother areasmatteranything thattakes upspace andhas massdivergentboundarymovesapartconvergentboundarymovestogether10010 x10ashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionsubductionwhen oneplate slidesunderanotherhurricanelarge swirlingstorm thatforms overoceansmantlethickestlayer ofearthvolcanicbombslargeprojectilesthrownthroughthe airmagmamoltenrock underEarth’ssurfacesecondaryconelava buildsup here inthe shapeof a conefaultbreak inearth'scrustpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfaceinnercoresolid ironandnickelPangeasupercontinentmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustriftvalleysform heredivergentboundarytransformboundaryplatesslide pasteachothercrustouter,thinnestlayer ofearthmountainsform hereconvergentboundarylavamoltenrock aboveEarth’ssurfacecratercircularbasin ordepressionsecondaryventmagmacan reachthe surfaceinother areasmatteranything thattakes upspace andhas massdivergentboundarymovesapartconvergentboundarymovestogether10010 x10ashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionsubductionwhen oneplate slidesunderanotherhurricanelarge swirlingstorm thatforms overoceansmantlethickestlayer ofearthvolcanicbombslargeprojectilesthrownthroughthe airmagmamoltenrock underEarth’ssurfacesecondaryconelava buildsup here inthe shapeof a conefaultbreak inearth'scrustpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfaceinnercoresolid ironandnickelPangeasupercontinent

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