mountainsform hereconvergentboundaryhurricanelarge swirlingstorm thatforms overoceansashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptioncratercircularbasin ordepressionsecondaryventmagmacan reachthe surfaceinother areasfaultbreak inearth'scrustsecondaryconelava buildsup here inthe shapeof a conemantlethickestlayer ofearthriftvalleysform heredivergentboundarydivergentboundarymovesaparttransformboundaryplatesslide pasteachotherinnercoresolid ironandnickellavamoltenrock aboveEarth’ssurfacePangeasupercontinentconvergentboundarymovestogether10010 x10mainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacevolcanicbombslargeprojectilesthrownthroughthe airsubductionwhen oneplate slidesunderanotherpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustcrustouter,thinnestlayer ofearthmatteranything thattakes upspace andhas massmagmamoltenrock underEarth’ssurfacemountainsform hereconvergentboundaryhurricanelarge swirlingstorm thatforms overoceansashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptioncratercircularbasin ordepressionsecondaryventmagmacan reachthe surfaceinother areasfaultbreak inearth'scrustsecondaryconelava buildsup here inthe shapeof a conemantlethickestlayer ofearthriftvalleysform heredivergentboundarydivergentboundarymovesaparttransformboundaryplatesslide pasteachotherinnercoresolid ironandnickellavamoltenrock aboveEarth’ssurfacePangeasupercontinentconvergentboundarymovestogether10010 x10mainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacevolcanicbombslargeprojectilesthrownthroughthe airsubductionwhen oneplate slidesunderanotherpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustcrustouter,thinnestlayer ofearthmatteranything thattakes upspace andhas massmagmamoltenrock underEarth’ssurface

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