PROPERTIESOFMINERALSColor,hardness,luster,density,cleavageIGNEOUSROCKSolidifiesfrom moltenrock deepinside EarthRAIN FALLS FROMCLOUDS & FORMSSTREAMS & RIVERSTHAT PROVIDEDRINKING WATERFOR HUMANS,PLANTS & WILDLIFEHow theEarth'sspheresinteractAERIALPHOTOGRAPHYPhotographstaken bycamerasmounted inairplanesThe way thata mineralbreaks alongsmooth flatplanes.CLEAVAGETOPOGRAPHICMAPSThese havecontour lines toshow elevation,relief, andslope.CRYOSPHEREThe frozenpart of thehydrosphereOUTERCORELiquid iron &nickel layerthat liesbeneath themantleBIOSPHEREThe parts ofearth thatcontain alllivingorganismsMINERALA naturallyoccurring solid,inorganicsubstance that hasa crystallinestructureCHARACTERSOF MINERALSA solid, naturallyoccurring, forms byinorganic processes,crystal structure, anda definite chemicalcomposition.THECRUSTThe rockthat formsEarth'souter layerFORM WHENEXISTINGROCKS ARECHANGED BYHEAT &PRESSUREMetamorphicRocksThe ability ofa mineral toresist beingscratchedHARDNESSSATELLITEIMAGERYMaps of Earthusingcomputers thatinterpretsatelliteimageryCRYSTALTheexternalshape ofa mineralGEOSPHEREThe part ofEarthcontainingrocks &mineralsTHE ROCKJUSTBELOW THEEARTH'SCRUSTTheMantleCONVECTIONCURRENTSCarry hot, solidrock of themantle outwardand cooled,solid rockinwardINNERCOREThe deepestlayer onEarth, madeup of iron &nickel3%Thedistributionof freshwater onEarthATMOSPHEREThe thinenvelope ofgases thatforms earth'souter layerSEDIMENTARYROCKLayeredrock suchaslimestoneHOW THEROCKCYCLEWORKSMagma sent to the Earth'ssurface cools & hardens toform an igneous rock. Therock breaks into smallpieces of sediment &slowly build and hardensinto sedimentary rock. Therock goes deep into thearth's crust Heat &pressure get intense, thePROPERTIESOFMINERALSColor,hardness,luster,density,cleavageIGNEOUSROCKSolidifiesfrom moltenrock deepinside EarthRAIN FALLS FROMCLOUDS & FORMSSTREAMS & RIVERSTHAT PROVIDEDRINKING WATERFOR HUMANS,PLANTS & WILDLIFEHow theEarth'sspheresinteractAERIALPHOTOGRAPHYPhotographstaken bycamerasmounted inairplanesThe way thata mineralbreaks alongsmooth flatplanes.CLEAVAGETOPOGRAPHICMAPSThese havecontour lines toshow elevation,relief, andslope.CRYOSPHEREThe frozenpart of thehydrosphereOUTERCORELiquid iron &nickel layerthat liesbeneath themantleBIOSPHEREThe parts ofearth thatcontain alllivingorganismsMINERALA naturallyoccurring solid,inorganicsubstance that hasa crystallinestructureCHARACTERSOF MINERALSA solid, naturallyoccurring, forms byinorganic processes,crystal structure, anda definite chemicalcomposition.THECRUSTThe rockthat formsEarth'souter layerFORM WHENEXISTINGROCKS ARECHANGED BYHEAT &PRESSUREMetamorphicRocksThe ability ofa mineral toresist beingscratchedHARDNESSSATELLITEIMAGERYMaps of Earthusingcomputers thatinterpretsatelliteimageryCRYSTALTheexternalshape ofa mineralGEOSPHEREThe part ofEarthcontainingrocks &mineralsTHE ROCKJUSTBELOW THEEARTH'SCRUSTTheMantleCONVECTIONCURRENTSCarry hot, solidrock of themantle outwardand cooled,solid rockinwardINNERCOREThe deepestlayer onEarth, madeup of iron &nickel3%Thedistributionof freshwater onEarthATMOSPHEREThe thinenvelope ofgases thatforms earth'souter layerSEDIMENTARYROCKLayeredrock suchaslimestoneHOW THEROCKCYCLEWORKSMagma sent to the Earth'ssurface cools & hardens toform an igneous rock. Therock breaks into smallpieces of sediment &slowly build and hardensinto sedimentary rock. Therock goes deep into thearth's crust Heat &pressure get intense, the

GEOLOGY - 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. Color, hardness,luster, density, cleavage
    PROPERTIES OF MINERALS
  2. Solidifies from molten rock deep inside Earth
    IGNEOUS ROCK
  3. How the Earth's spheres interact
    RAIN FALLS FROM CLOUDS & FORMS STREAMS & RIVERS THAT PROVIDE DRINKING WATER FOR HUMANS, PLANTS & WILDLIFE
  4. Photographs taken by cameras mounted in airplanes
    AERIAL PHOTOGRAPHY
  5. CLEAVAGE
    The way that a mineral breaks along smooth flat planes.
  6. These have contour lines to show elevation, relief, and slope.
    TOPOGRAPHIC MAPS
  7. The frozen part of the hydrosphere
    CRYOSPHERE
  8. Liquid iron & nickel layer that lies beneath the mantle
    OUTER CORE
  9. The parts of earth that contain all living organisms
    BIOSPHERE
  10. A naturally occurring solid, inorganic substance that has a crystalline structure
    MINERAL
  11. A solid, naturally occurring, forms by inorganic processes, crystal structure, and a definite chemical composition.
    CHARACTERS OF MINERALS
  12. The rock that forms Earth's outer layer
    THE CRUST
  13. Metamorphic Rocks
    FORM WHEN EXISTING ROCKS ARE CHANGED BY HEAT & PRESSURE
  14. HARDNESS
    The ability of a mineral to resist being scratched
  15. Maps of Earth using computers that interpret satellite imagery
    SATELLITE IMAGERY
  16. The external shape of a mineral
    CRYSTAL
  17. The part of Earth containing rocks & minerals
    GEOSPHERE
  18. The Mantle
    THE ROCK JUST BELOW THE EARTH'S CRUST
  19. Carry hot, solid rock of the mantle outward and cooled, solid rock inward
    CONVECTION CURRENTS
  20. The deepest layer on Earth, made up of iron & nickel
    INNER CORE
  21. The distribution of fresh water on Earth
    3%
  22. The thin envelope of gases that forms earth's outer layer
    ATMOSPHERE
  23. Layered rock such as limestone
    SEDIMENTARY ROCK
  24. Magma sent to the Earth's surface cools & hardens to form an igneous rock. The rock breaks into small pieces of sediment & slowly build and hardens into sedimentary rock. The rock goes deep into th earth's crust Heat & pressure get intense, the
    HOW THE ROCK CYCLE WORKS