mountainsform hereconvergentboundarymainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesecondaryventmagmacan reachthe surfaceinother areaslavamoltenrock aboveEarth’ssurfacefaultbreak inearth'scrustsubductionwhen oneplate slidesunderanotherriftvalleysform heredivergentboundarymagmamoltenrock underEarth’ssurfacevolcanicbombslargeprojectilesthrownthroughthe airmatteranything thattakes upspace andhas massashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptiontransformboundaryplatesslide pasteachothercratercircularbasin ordepressionpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomantlethickestlayer ofearthPangeasupercontinentmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustdivergentboundarymovesapartcrustouter,thinnestlayer ofearthsecondaryconelava buildsup here inthe shapeof a conehurricanelarge swirlingstorm thatforms overoceansconvergentboundarymovestogether10010 x10innercoresolid ironandnickelmountainsform hereconvergentboundarymainventthe weak pointin Earth’s crust wherehotmagma rises fromthemagma chamber andreachesthe surfacesecondaryventmagmacan reachthe surfaceinother areaslavamoltenrock aboveEarth’ssurfacefaultbreak inearth'scrustsubductionwhen oneplate slidesunderanotherriftvalleysform heredivergentboundarymagmamoltenrock underEarth’ssurfacevolcanicbombslargeprojectilesthrownthroughthe airmatteranything thattakes upspace andhas massashcloudsmall pieces ofpulverized rock,minerals,and volcanicglass createdduring eruptiontransformboundaryplatesslide pasteachothercratercircularbasin ordepressionpyroclasticflowfast movingcurrent of hotgasand rock thatmoves awayfrom a volcanomantlethickestlayer ofearthPangeasupercontinentmagmachamberlargeundergroundpool of moltenrock sittingunderneathEarth’s crustdivergentboundarymovesapartcrustouter,thinnestlayer ofearthsecondaryconelava buildsup here inthe shapeof a conehurricanelarge swirlingstorm thatforms overoceansconvergentboundarymovestogether10010 x10innercoresolid ironandnickel

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