IntrusiveIgneousrocks coolinginside theearthCompactionRocks aresquishedvery closetogetherIgneousRockPictureCoolingMoltenrocksturning backinto solidsCrystalsThese formbased onhow fast orslow moltenrock coolsSedimentName for thesmall bits ofbroken rocksExtrusiveIgneousrocks coolingon thesurface ofthe earthExtinctionGreat lossof life atone timeMagmaMoltenrockbelowgroundMetamorphicRock PictureEraThe middleamount ofgeologictimeMeltingAddingextremeheatcauses thisEonThe longestamount ofgeologictimeIgneousRockDescriptionMolten rockthat hascooled backinto a solidformPeriodThe shortestamount ofgeologictimeWeatheringThe breakingdown ofrocks intosmall bitsSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceLayersSedimentaryrocks usuallyhave verydefined_____.SedimentaryRockPictureMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureLavaMoltenrockabovegroundErosionMovement ofsedimentfrom oneplace toanotherHeatThermalenergythat canmelt rockPressureTheweight ofthe rocksabove itIntrusiveIgneousrocks coolinginside theearthCompactionRocks aresquishedvery closetogetherIgneousRockPictureCoolingMoltenrocksturning backinto solidsCrystalsThese formbased onhow fast orslow moltenrock coolsSedimentName for thesmall bits ofbroken rocksExtrusiveIgneousrocks coolingon thesurface ofthe earthExtinctionGreat lossof life atone timeMagmaMoltenrockbelowgroundMetamorphicRock PictureEraThe middleamount ofgeologictimeMeltingAddingextremeheatcauses thisEonThe longestamount ofgeologictimeIgneousRockDescriptionMolten rockthat hascooled backinto a solidformPeriodThe shortestamount ofgeologictimeWeatheringThe breakingdown ofrocks intosmall bitsSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceLayersSedimentaryrocks usuallyhave verydefined_____.SedimentaryRockPictureMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureLavaMoltenrockabovegroundErosionMovement ofsedimentfrom oneplace toanotherHeatThermalenergythat canmelt rockPressureTheweight ofthe rocksabove it

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. Igneous rocks cooling inside the earth
    Intrusive
  2. Rocks are squished very close together
    Compaction

  3. Igneous Rock Picture
  4. Molten rocks turning back into solids
    Cooling
  5. These form based on how fast or slow molten rock cools
    Crystals
  6. Name for the small bits of broken rocks
    Sediment
  7. Igneous rocks cooling on the surface of the earth
    Extrusive
  8. Great loss of life at one time
    Extinction
  9. Molten rock below ground
    Magma

  10. Metamorphic Rock Picture
  11. The middle amount of geologic time
    Era
  12. Adding extreme heat causes this
    Melting
  13. The longest amount of geologic time
    Eon
  14. Molten rock that has cooled back into a solid form
    Igneous Rock Description
  15. The shortest amount of geologic time
    Period
  16. The breaking down of rocks into small bits
    Weathering
  17. Sediment that has been compacted into one solid piece
    Sedimentary Rock Description
  18. Sedimentary rocks usually have very defined _____.
    Layers

  19. Sedimentary Rock Picture
  20. Existing rocks that have changed due to heat and pressure
    Metamorphic Rock Description
  21. Molten rock above ground
    Lava
  22. Movement of sediment from one place to another
    Erosion
  23. Thermal energy that can melt rock
    Heat
  24. The weight of the rocks above it
    Pressure