WeatheringThe breakingdown ofrocks intosmall bitsLayersSedimentaryrocks usuallyhave verydefined_____.CoolingMoltenrocksturning backinto solidsCompactionRocks aresquishedvery closetogetherExtinctionGreat lossof life atone timeSedimentName for thesmall bits ofbroken rocksIntrusiveIgneousrocks coolinginside theearthIgneousRockPictureMagmaMoltenrockbelowgroundIgneousRockDescriptionMolten rockthat hascooled backinto a solidformPressureTheweight ofthe rocksabove itMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureMetamorphicRock PictureHeatThermalenergythat canmelt rockEraThe middleamount ofgeologictimeLavaMoltenrockabovegroundSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceSedimentaryRockPicturePeriodThe shortestamount ofgeologictimeCrystalsThese formbased onhow fast orslow moltenrock coolsEonThe longestamount ofgeologictimeMeltingAddingextremeheatcauses thisErosionMovement ofsedimentfrom oneplace toanotherExtrusiveIgneousrocks coolingon thesurface ofthe earthWeatheringThe breakingdown ofrocks intosmall bitsLayersSedimentaryrocks usuallyhave verydefined_____.CoolingMoltenrocksturning backinto solidsCompactionRocks aresquishedvery closetogetherExtinctionGreat lossof life atone timeSedimentName for thesmall bits ofbroken rocksIntrusiveIgneousrocks coolinginside theearthIgneousRockPictureMagmaMoltenrockbelowgroundIgneousRockDescriptionMolten rockthat hascooled backinto a solidformPressureTheweight ofthe rocksabove itMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureMetamorphicRock PictureHeatThermalenergythat canmelt rockEraThe middleamount ofgeologictimeLavaMoltenrockabovegroundSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceSedimentaryRockPicturePeriodThe shortestamount ofgeologictimeCrystalsThese formbased onhow fast orslow moltenrock coolsEonThe longestamount ofgeologictimeMeltingAddingextremeheatcauses thisErosionMovement ofsedimentfrom oneplace toanotherExtrusiveIgneousrocks coolingon thesurface ofthe earth

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. The breaking down of rocks into small bits
    Weathering
  2. Sedimentary rocks usually have very defined _____.
    Layers
  3. Molten rocks turning back into solids
    Cooling
  4. Rocks are squished very close together
    Compaction
  5. Great loss of life at one time
    Extinction
  6. Name for the small bits of broken rocks
    Sediment
  7. Igneous rocks cooling inside the earth
    Intrusive

  8. Igneous Rock Picture
  9. Molten rock below ground
    Magma
  10. Molten rock that has cooled back into a solid form
    Igneous Rock Description
  11. The weight of the rocks above it
    Pressure
  12. Existing rocks that have changed due to heat and pressure
    Metamorphic Rock Description

  13. Metamorphic Rock Picture
  14. Thermal energy that can melt rock
    Heat
  15. The middle amount of geologic time
    Era
  16. Molten rock above ground
    Lava
  17. Sediment that has been compacted into one solid piece
    Sedimentary Rock Description

  18. Sedimentary Rock Picture
  19. The shortest amount of geologic time
    Period
  20. These form based on how fast or slow molten rock cools
    Crystals
  21. The longest amount of geologic time
    Eon
  22. Adding extreme heat causes this
    Melting
  23. Movement of sediment from one place to another
    Erosion
  24. Igneous rocks cooling on the surface of the earth
    Extrusive