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Structure's of the Earth

Review of Chapter 18

AB
METAMORPHISMROCKS UNDERGO CHANGES IN COMPOSITION AND TEXTURE
WEATHERINGBREAKS ROCKS INTO SMALLER PIECES OR CHANGES THEIR CHEMICAL COMPOSITION
FAULTA FRACTURE IN A MASS OF ROCK IN WHICH MOVEMENT OCCURS
MORAINSRIDGES OF BOULDERS AND ROCK FRAGMENTS DEPOSITED BY A GLACIER
MINERALSHAVE A DEFINITE CHEMICAL COMPOSITION AND MOLECULAR STRUCTURE
INTRUSIVEMAGMA THAT COOLED SLOWLY, LARGE MINERAL GRAINS
EXTRUSIVEMAGMA THAT COOLED QUICKLY, FINE MINERAL GRAINS
LANDSLIDEWEATHERED ROCK AND SOIL ARE SUDDENLY LOOSENED AND SLIP DOWN SLOPE
WATERSHEDLAND THAT SUPPLIES WATER FOR A LARGE NETWORK OF STREAMS
WATER TABLETOP OF THE SATURATION ZONE IN PERMEABLE ROCK
MUDFLOWOCCURS IN DRY MTN REGIONS WHEN HEAVY RAINS SATURATE SEDIMENT MOVING IT DOWN SLOPE
CREEPSLOW MASS MOVEMENT THAT TAKES PLACE ON MOST SLOPES
CAVERNSMAY FORM WHEN GROUNDWATER DISSOLVES LIMESTONE
GRANITEEXAMPLE OF INTRUSIVE IGNEOUS ROCK
OBSIDIANEXAMPLE OF EXTRUSIVE IGNEOUS ROCK
FOLIATEDMETAMORPHIC ROCK WITH PARALLEL MINERAL GRAIN LAYERS
NONFOLIATEDMETAMORPHIC ROCKS WITH NO MINERAL GRAIN LAYERS
GLACIERSMASSES OF FLOWING ICE
LOESSTYPE OF SAND DEPOSIT CAUSED BY WIND
LIMESTONEEXAMPLE OF A SEDIMENTARY ROCK

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