divergentboundarymovesapartsecondaryconelava buildsup here inthe shapeof a conevolcanicbombslargeprojectilesthrownthroughthe airtransformboundaryplatesslide pasteachotherriftvalleysform heredivergentboundarymagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustlavamoltenrock aboveEarth’ssurface10010 x10magmamoltenrock underEarth’ssurfacepyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanosubductionwhen oneplate slidesunderanotherinnercoresolid ironandnickelashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionconvergentboundarymovestogetherfaultbreak inearth'scrusthurricanelarge swirlingstorm thatforms overoceanscratercircularbasin ordepressionmantlethickestlayer ofearthPangeasupercontinentmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesecondaryventmagmacan reachthe surfaceinother areasmatteranything thattakes upspace andhas massmountainsform hereconvergentboundarycrustouter,thinnestlayer ofearthdivergentboundarymovesapartsecondaryconelava buildsup here inthe shapeof a conevolcanicbombslargeprojectilesthrownthroughthe airtransformboundaryplatesslide pasteachotherriftvalleysform heredivergentboundarymagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustlavamoltenrock aboveEarth’ssurface10010 x10magmamoltenrock underEarth’ssurfacepyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanosubductionwhen oneplate slidesunderanotherinnercoresolid ironandnickelashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionconvergentboundarymovestogetherfaultbreak inearth'scrusthurricanelarge swirlingstorm thatforms overoceanscratercircularbasin ordepressionmantlethickestlayer ofearthPangeasupercontinentmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesecondaryventmagmacan reachthe surfaceinother areasmatteranything thattakes upspace andhas massmountainsform hereconvergentboundarycrustouter,thinnestlayer ofearth

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