3%Thedistributionof freshwater onEarthSATELLITEIMAGERYMaps of Earthusingcomputers thatinterpretsatelliteimageryBIOSPHEREThe parts ofearth thatcontain alllivingorganismsATMOSPHEREThe thinenvelope ofgases thatforms earth'souter layerRAIN FALLS FROMCLOUDS & FORMSSTREAMS & RIVERSTHAT PROVIDEDRINKING WATERFOR HUMANS,PLANTS & WILDLIFEHow theEarth'sspheresinteractOUTERCORELiquid iron &nickel layerthat liesbeneath themantleThe way thata mineralbreaks alongsmooth flatplanes.CLEAVAGECRYOSPHEREThe frozenpart of thehydrosphereCHARACTERSOF MINERALSA solid, naturallyoccurring, forms byinorganic processes,crystal structure, anda definite chemicalcomposition.The ability ofa mineral toresist beingscratchedHARDNESSAERIALPHOTOGRAPHYPhotographstaken bycamerasmounted inairplanesCRYSTALTheexternalshape ofa mineralIGNEOUSROCKSolidifiesfrom moltenrock deepinside EarthGEOSPHEREThe part ofEarthcontainingrocks &mineralsINNERCOREThe deepestlayer onEarth, madeup of iron &nickelSEDIMENTARYROCKLayeredrock suchaslimestoneTOPOGRAPHICMAPSThese havecontour lines toshow elevation,relief, andslope.THE ROCKJUSTBELOW THEEARTH'SCRUSTTheMantleFORM WHENEXISTINGROCKS ARECHANGED BYHEAT &PRESSUREMetamorphicRocksCONVECTIONCURRENTSCarry hot, solidrock of themantle outwardand cooled,solid rockinwardTHECRUSTThe rockthat formsEarth'souter layerPROPERTIESOFMINERALSColor,hardness,luster,density,cleavageMINERALA naturallyoccurring solid,inorganicsubstance that hasa crystallinestructureHOW 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, the3%Thedistributionof freshwater onEarthSATELLITEIMAGERYMaps of Earthusingcomputers thatinterpretsatelliteimageryBIOSPHEREThe parts ofearth thatcontain alllivingorganismsATMOSPHEREThe thinenvelope ofgases thatforms earth'souter layerRAIN FALLS FROMCLOUDS & FORMSSTREAMS & RIVERSTHAT PROVIDEDRINKING WATERFOR HUMANS,PLANTS & WILDLIFEHow theEarth'sspheresinteractOUTERCORELiquid iron &nickel layerthat liesbeneath themantleThe way thata mineralbreaks alongsmooth flatplanes.CLEAVAGECRYOSPHEREThe frozenpart of thehydrosphereCHARACTERSOF MINERALSA solid, naturallyoccurring, forms byinorganic processes,crystal structure, anda definite chemicalcomposition.The ability ofa mineral toresist beingscratchedHARDNESSAERIALPHOTOGRAPHYPhotographstaken bycamerasmounted inairplanesCRYSTALTheexternalshape ofa mineralIGNEOUSROCKSolidifiesfrom moltenrock deepinside EarthGEOSPHEREThe part ofEarthcontainingrocks &mineralsINNERCOREThe deepestlayer onEarth, madeup of iron &nickelSEDIMENTARYROCKLayeredrock suchaslimestoneTOPOGRAPHICMAPSThese havecontour lines toshow elevation,relief, andslope.THE ROCKJUSTBELOW THEEARTH'SCRUSTTheMantleFORM WHENEXISTINGROCKS ARECHANGED BYHEAT &PRESSUREMetamorphicRocksCONVECTIONCURRENTSCarry hot, solidrock of themantle outwardand cooled,solid rockinwardTHECRUSTThe rockthat formsEarth'souter layerPROPERTIESOFMINERALSColor,hardness,luster,density,cleavageMINERALA naturallyoccurring solid,inorganicsubstance that hasa crystallinestructureHOW 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. The distribution of fresh water on Earth
    3%
  2. Maps of Earth using computers that interpret satellite imagery
    SATELLITE IMAGERY
  3. The parts of earth that contain all living organisms
    BIOSPHERE
  4. The thin envelope of gases that forms earth's outer layer
    ATMOSPHERE
  5. How the Earth's spheres interact
    RAIN FALLS FROM CLOUDS & FORMS STREAMS & RIVERS THAT PROVIDE DRINKING WATER FOR HUMANS, PLANTS & WILDLIFE
  6. Liquid iron & nickel layer that lies beneath the mantle
    OUTER CORE
  7. CLEAVAGE
    The way that a mineral breaks along smooth flat planes.
  8. The frozen part of the hydrosphere
    CRYOSPHERE
  9. A solid, naturally occurring, forms by inorganic processes, crystal structure, and a definite chemical composition.
    CHARACTERS OF MINERALS
  10. HARDNESS
    The ability of a mineral to resist being scratched
  11. Photographs taken by cameras mounted in airplanes
    AERIAL PHOTOGRAPHY
  12. The external shape of a mineral
    CRYSTAL
  13. Solidifies from molten rock deep inside Earth
    IGNEOUS ROCK
  14. The part of Earth containing rocks & minerals
    GEOSPHERE
  15. The deepest layer on Earth, made up of iron & nickel
    INNER CORE
  16. Layered rock such as limestone
    SEDIMENTARY ROCK
  17. These have contour lines to show elevation, relief, and slope.
    TOPOGRAPHIC MAPS
  18. The Mantle
    THE ROCK JUST BELOW THE EARTH'S CRUST
  19. Metamorphic Rocks
    FORM WHEN EXISTING ROCKS ARE CHANGED BY HEAT & PRESSURE
  20. Carry hot, solid rock of the mantle outward and cooled, solid rock inward
    CONVECTION CURRENTS
  21. The rock that forms Earth's outer layer
    THE CRUST
  22. Color, hardness,luster, density, cleavage
    PROPERTIES OF MINERALS
  23. A naturally occurring solid, inorganic substance that has a crystalline structure
    MINERAL
  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