HeatThermalenergythat canmelt rockPressureTheweight ofthe rocksabove itEraThe middleamount ofgeologictimeMeltingAddingextremeheatcauses thisIgneousRockPictureCompactionRocks aresquishedvery closetogetherSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceErosionMovement ofsedimentfrom oneplace toanotherCoolingMoltenrocksturning backinto solidsWeatheringThe breakingdown ofrocks intosmall bitsMetamorphicRock PictureEonThe longestamount ofgeologictimeLayersSedimentaryrocks usuallyhave verydefined_____.IgneousRockDescriptionMolten rockthat hascooled backinto a solidformMagmaMoltenrockbelowgroundCrystalsThese formbased onhow fast orslow moltenrock coolsIntrusiveIgneousrocks coolinginside theearthSedimentaryRockPictureExtrusiveIgneousrocks coolingon thesurface ofthe earthMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureLavaMoltenrockabovegroundPeriodThe shortestamount ofgeologictimeExtinctionGreat lossof life atone timeSedimentName for thesmall bits ofbroken rocksHeatThermalenergythat canmelt rockPressureTheweight ofthe rocksabove itEraThe middleamount ofgeologictimeMeltingAddingextremeheatcauses thisIgneousRockPictureCompactionRocks aresquishedvery closetogetherSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceErosionMovement ofsedimentfrom oneplace toanotherCoolingMoltenrocksturning backinto solidsWeatheringThe breakingdown ofrocks intosmall bitsMetamorphicRock PictureEonThe longestamount ofgeologictimeLayersSedimentaryrocks usuallyhave verydefined_____.IgneousRockDescriptionMolten rockthat hascooled backinto a solidformMagmaMoltenrockbelowgroundCrystalsThese formbased onhow fast orslow moltenrock coolsIntrusiveIgneousrocks coolinginside theearthSedimentaryRockPictureExtrusiveIgneousrocks coolingon thesurface ofthe earthMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureLavaMoltenrockabovegroundPeriodThe shortestamount ofgeologictimeExtinctionGreat lossof life atone timeSedimentName for thesmall bits ofbroken rocks

Geology Unit Review - 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. Thermal energy that can melt rock
    Heat
  2. The weight of the rocks above it
    Pressure
  3. The middle amount of geologic time
    Era
  4. Adding extreme heat causes this
    Melting

  5. Igneous Rock Picture
  6. Rocks are squished very close together
    Compaction
  7. Sediment that has been compacted into one solid piece
    Sedimentary Rock Description
  8. Movement of sediment from one place to another
    Erosion
  9. Molten rocks turning back into solids
    Cooling
  10. The breaking down of rocks into small bits
    Weathering

  11. Metamorphic Rock Picture
  12. The longest amount of geologic time
    Eon
  13. Sedimentary rocks usually have very defined _____.
    Layers
  14. Molten rock that has cooled back into a solid form
    Igneous Rock Description
  15. Molten rock below ground
    Magma
  16. These form based on how fast or slow molten rock cools
    Crystals
  17. Igneous rocks cooling inside the earth
    Intrusive

  18. Sedimentary Rock Picture
  19. Igneous rocks cooling on the surface of the earth
    Extrusive
  20. Existing rocks that have changed due to heat and pressure
    Metamorphic Rock Description
  21. Molten rock above ground
    Lava
  22. The shortest amount of geologic time
    Period
  23. Great loss of life at one time
    Extinction
  24. Name for the small bits of broken rocks
    Sediment