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Chap 06 Rocks

AB
batholithlarge puton of intrusive igneous rock forming the core of a mountain
cementationprocess by which particles are bound as minerals fill in spaces
chemical rockformed by precipitation of minerals from solution caused by evaporation or chemical action
clastic rockformed from fragments of other rock moved and collected by running water
contact metamorphismhot magma moves into existing rock heating and changing it
deformheat from friction stress pressure causes a rock to change shape
deformational metamorphismoccurs at low temperatures caused by pressure caused by stress and friction
dikeintrusive rock that crosses through existing rock layers via cracks
extrusive rockmagma cools quickly on surface with fine grain texture of small crystals
felsicthick slow moving magma with large amounts of silica forms quartz and orthoclase feldspar
foliationwavy parallel bands characteristic of metamorphic rocks
fossilremains impression evidence of plant or aninmal remains preserved in rock
geodespheres of silca rock lined with crystals formed of dissolved minerals
gneissmetamorphized granites and conglomerates
granitecoarse grained intrusive igneous rock
igneous rockformed by cooling and hardening of hot molten rock
intrusive rockmagma cools beneath slowly surface with coarse grain texture of large crystals
maficthinner more fluid magma with large amounts of iron & magnesium forms horneblend and biotite
magmahot molten rock
marblemetamorphized limestone
metamorphic rockformed by effect of heat and pressure on other rocks
metamorphismprocess by which rock structure is changed by pressure heat and moisture
obsidianquick cooled glassy extrusive volcanic rock
organic rockforms from sediments of the remains of plants and animals
plutonigneous intrusions formed when magma cools inside Earth
pumicequick cooled extrusive rock hardened as steam and gases bubbled
quartzitemetaqmorphic sandstone
regional metamorphismoccurs during mountain building movements of crust
rockgroup of minerals bound together
rock cyclerepeated series of events by which rock gradually and continually cahnges
schistmetamorphized shales and basalts
sedimentmaterials such as rock fragments plant and animal remains that settle out of water
sedimentary rockformed by compaction and cementation of layers of sediments
sillintrusive rock that runs parallel to existing rock layers via cracks
slatemetamorphized shale
stratificationarrangement of sedimentary rock in visible layers


Science Instructor
Scarsdale, NY

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