PROPERTIESOFMINERALSColor,hardness,luster,density,cleavageAERIALPHOTOGRAPHYPhotographstaken bycamerasmounted inairplanesCRYSTALTheexternalshape ofa mineralBIOSPHEREThe parts ofearth thatcontain alllivingorganismsGEOSPHEREThe part ofEarthcontainingrocks &mineralsINNERCOREThe deepestlayer onEarth, madeup of iron &nickel3%Thedistributionof freshwater onEarthCHARACTERSOF MINERALSA solid, naturallyoccurring, forms byinorganic processes,crystal structure, anda definite chemicalcomposition.SEDIMENTARYROCKLayeredrock suchaslimestoneFORM WHENEXISTINGROCKS ARECHANGED BYHEAT &PRESSUREMetamorphicRocksTHECRUSTThe rockthat formsEarth'souter layerOUTERCORELiquid iron &nickel layerthat liesbeneath themantleThe ability ofa mineral toresist beingscratchedHARDNESSThe way thata mineralbreaks alongsmooth flatplanes.CLEAVAGECONVECTIONCURRENTSCarry hot, solidrock of themantle outwardand cooled,solid rockinwardTHE ROCKJUSTBELOW THEEARTH'SCRUSTTheMantleRAIN FALLS FROMCLOUDS & FORMSSTREAMS & RIVERSTHAT PROVIDEDRINKING WATERFOR HUMANS,PLANTS & WILDLIFEHow theEarth'sspheresinteractMINERALA naturallyoccurring solid,inorganicsubstance that hasa crystallinestructureTOPOGRAPHICMAPSThese havecontour lines toshow elevation,relief, andslope.SATELLITEIMAGERYMaps of Earthusingcomputers thatinterpretsatelliteimageryIGNEOUSROCKSolidifiesfrom moltenrock deepinside EarthATMOSPHEREThe thinenvelope ofgases thatforms earth'souter layerHOW 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, theCRYOSPHEREThe frozenpart of thehydrospherePROPERTIESOFMINERALSColor,hardness,luster,density,cleavageAERIALPHOTOGRAPHYPhotographstaken bycamerasmounted inairplanesCRYSTALTheexternalshape ofa mineralBIOSPHEREThe parts ofearth thatcontain alllivingorganismsGEOSPHEREThe part ofEarthcontainingrocks &mineralsINNERCOREThe deepestlayer onEarth, madeup of iron &nickel3%Thedistributionof freshwater onEarthCHARACTERSOF MINERALSA solid, naturallyoccurring, forms byinorganic processes,crystal structure, anda definite chemicalcomposition.SEDIMENTARYROCKLayeredrock suchaslimestoneFORM WHENEXISTINGROCKS ARECHANGED BYHEAT &PRESSUREMetamorphicRocksTHECRUSTThe rockthat formsEarth'souter layerOUTERCORELiquid iron &nickel layerthat liesbeneath themantleThe ability ofa mineral toresist beingscratchedHARDNESSThe way thata mineralbreaks alongsmooth flatplanes.CLEAVAGECONVECTIONCURRENTSCarry hot, solidrock of themantle outwardand cooled,solid rockinwardTHE ROCKJUSTBELOW THEEARTH'SCRUSTTheMantleRAIN FALLS FROMCLOUDS & FORMSSTREAMS & RIVERSTHAT PROVIDEDRINKING WATERFOR HUMANS,PLANTS & WILDLIFEHow theEarth'sspheresinteractMINERALA naturallyoccurring solid,inorganicsubstance that hasa crystallinestructureTOPOGRAPHICMAPSThese havecontour lines toshow elevation,relief, andslope.SATELLITEIMAGERYMaps of Earthusingcomputers thatinterpretsatelliteimageryIGNEOUSROCKSolidifiesfrom moltenrock deepinside EarthATMOSPHEREThe thinenvelope ofgases thatforms earth'souter layerHOW 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, theCRYOSPHEREThe frozenpart of thehydrosphere

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