riftvalleysform heredivergentboundarycrustouter,thinnestlayer ofearth10010 x10matteranything thattakes upspace andhas massmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesubductionwhen oneplate slidesunderanothermantlethickestlayer ofearthmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustPangeasupercontinentmountainsform hereconvergentboundarycratercircularbasin ordepressionhurricanelarge swirlingstorm thatforms overoceanspyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanotransformboundaryplatesslide pasteachotherinnercoresolid ironandnickelvolcanicbombslargeprojectilesthrownthroughthe airconvergentboundarymovestogetherashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionsecondaryventmagmacan reachthe surfaceinother areassecondaryconelava buildsup here inthe shapeof a conedivergentboundarymovesapartmagmamoltenrock underEarth’ssurfacefaultbreak inearth'scrustlavamoltenrock aboveEarth’ssurfaceriftvalleysform heredivergentboundarycrustouter,thinnestlayer ofearth10010 x10matteranything thattakes upspace andhas massmainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesubductionwhen oneplate slidesunderanothermantlethickestlayer ofearthmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustPangeasupercontinentmountainsform hereconvergentboundarycratercircularbasin ordepressionhurricanelarge swirlingstorm thatforms overoceanspyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanotransformboundaryplatesslide pasteachotherinnercoresolid ironandnickelvolcanicbombslargeprojectilesthrownthroughthe airconvergentboundarymovestogetherashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptionsecondaryventmagmacan reachthe surfaceinother areassecondaryconelava buildsup here inthe shapeof a conedivergentboundarymovesapartmagmamoltenrock underEarth’ssurfacefaultbreak inearth'scrustlavamoltenrock aboveEarth’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. divergent boundary
    rift valleys form here
  2. outer, thinnest layer of earth
    crust
  3. 10 x 10
    100
  4. anything that takes up space and has mass
    matter
  5. the weak point in Earth’s crust where hot magma rises from the magma chamber and reaches the surface
    main vent
  6. when one plate slides under another
    subduction
  7. thickest layer of earth
    mantle
  8. large underground pool of molten rock sitting underneath Earth’s crust
    magma chamber
  9. supercontinent
    Pangea
  10. convergent boundary
    mountains form here
  11. circular basin or depression
    crater
  12. large swirling storm that forms over oceans
    hurricane
  13. fast moving current of hot gas and rock that moves away from a volcano
    pyroclastic flow
  14. plates slide past each other
    transform boundary
  15. solid iron and nickel
    inner core
  16. large projectiles thrown through the air
    volcanic bombs
  17. moves together
    convergent boundary
  18. small pieces of pulverized rock, minerals, and volcanic glass created during eruption
    ash cloud
  19. magma can reach the surface in other areas
    secondary vent
  20. lava builds up here in the shape of a cone
    secondary cone
  21. moves apart
    divergent boundary
  22. molten rock under Earth’s surface
    magma
  23. break in earth's crust
    fault
  24. molten rock above Earth’s surface
    lava