EonThe longestamount ofgeologictimeCrystalsThese formbased onhow fast orslow moltenrock coolsPeriodThe shortestamount ofgeologictimeMagmaMoltenrockbelowgroundHeatThermalenergythat canmelt rockPressureTheweight ofthe rocksabove itCoolingMoltenrocksturning backinto solidsEraThe middleamount ofgeologictimeErosionMovement ofsedimentfrom oneplace toanotherSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceExtrusiveIgneousrocks coolingon thesurface ofthe earthSedimentName for thesmall bits ofbroken rocksLayersSedimentaryrocks usuallyhave verydefined_____.CompactionRocks aresquishedvery closetogetherIgneousRockPictureExtinctionGreat lossof life atone timeSedimentaryRockPictureWeatheringThe breakingdown ofrocks intosmall bitsIntrusiveIgneousrocks coolinginside theearthMetamorphicRock PictureLavaMoltenrockabovegroundMeltingAddingextremeheatcauses thisIgneousRockDescriptionMolten rockthat hascooled backinto a solidformMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressureEonThe longestamount ofgeologictimeCrystalsThese formbased onhow fast orslow moltenrock coolsPeriodThe shortestamount ofgeologictimeMagmaMoltenrockbelowgroundHeatThermalenergythat canmelt rockPressureTheweight ofthe rocksabove itCoolingMoltenrocksturning backinto solidsEraThe middleamount ofgeologictimeErosionMovement ofsedimentfrom oneplace toanotherSedimentaryRockDescriptionSedimentthat has beencompactedinto one solidpieceExtrusiveIgneousrocks coolingon thesurface ofthe earthSedimentName for thesmall bits ofbroken rocksLayersSedimentaryrocks usuallyhave verydefined_____.CompactionRocks aresquishedvery closetogetherIgneousRockPictureExtinctionGreat lossof life atone timeSedimentaryRockPictureWeatheringThe breakingdown ofrocks intosmall bitsIntrusiveIgneousrocks coolinginside theearthMetamorphicRock PictureLavaMoltenrockabovegroundMeltingAddingextremeheatcauses thisIgneousRockDescriptionMolten rockthat hascooled backinto a solidformMetamorphicRockDescriptionExisting rocksthat havechanged dueto heat andpressure

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.


1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
  1. The longest amount of geologic time
    Eon
  2. These form based on how fast or slow molten rock cools
    Crystals
  3. The shortest amount of geologic time
    Period
  4. Molten rock below ground
    Magma
  5. Thermal energy that can melt rock
    Heat
  6. The weight of the rocks above it
    Pressure
  7. Molten rocks turning back into solids
    Cooling
  8. The middle amount of geologic time
    Era
  9. Movement of sediment from one place to another
    Erosion
  10. Sediment that has been compacted into one solid piece
    Sedimentary Rock Description
  11. Igneous rocks cooling on the surface of the earth
    Extrusive
  12. Name for the small bits of broken rocks
    Sediment
  13. Sedimentary rocks usually have very defined _____.
    Layers
  14. Rocks are squished very close together
    Compaction

  15. Igneous Rock Picture
  16. Great loss of life at one time
    Extinction

  17. Sedimentary Rock Picture
  18. The breaking down of rocks into small bits
    Weathering
  19. Igneous rocks cooling inside the earth
    Intrusive

  20. Metamorphic Rock Picture
  21. Molten rock above ground
    Lava
  22. Adding extreme heat causes this
    Melting
  23. Molten rock that has cooled back into a solid form
    Igneous Rock Description
  24. Existing rocks that have changed due to heat and pressure
    Metamorphic Rock Description