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Minerals and Rocks

Vocabulary

TermDefinition
inorganic matter that is not, or never was, living
crystal atoms in minerals are arranged in a pattern that is repeated over and over again
4 basic characteristics of minerals formed by natural processes; are inorganic solids; elements or compounds with a chemical composition unique to that mineral; crystal structures
color the most obvious, but one of the least reliable methods of identifying minerals
hardness measure of how easily a mineral can be scratched
luster how light s reflected from a mineral's surface
metallic minerals that look like metal
non-metallic minerals vary greatly in appearance and are usually described as shiny, pearly, waxy, glassy, etc.
cleavage and fracture refers to the way minerals break.
gems highly prized minerals because they are rare and beautiful
ores minerals that contain a useful substance that can be minded for money
igneous rock molten material from a volcano (lava) or from deep inside the earth (magma) which cools and hardens
extrusive igneous rock rock (volcanic) formed on the Earth's surface when molten rock flows out of the earth (lava) and cools quickly at the surface to form fine crystals.
intrusive igneous rock rock (plutonic) that is formed in the Earth when molten rock flows upward into the more solid part of the crust. these rocks have a coarse - grained texture. Example: granite
sedimentary rock can form from particles of rock, from remains of plants or animals, or from chemical reactions; classified by their composition and by the way they were formed
clastic sedimentary rocks sedimentary rocks that come from fragments of other rocks. Example: shale and sandstone
non-clastic organic rocks sedimentary rock that comes from the remains of organisms. Example: coal, limestone
non-clastic chemical sedimentary rocks sedimentary rock is formed when mineral grains dissolved in precipitated or left behind when a solution evaporates. Example: rock salt, gypsum
metamorphic rock forms from other rocks by heat and pressure and are classified by their texture
foliated metamorphic rock metamorphic rocks that have mineral grains within the rock that are arranged in nearly parallel layers. Example: slate, schist, and gneiss
non-foliated metamorphic rock metamorphic rocks that have mineral grains that change, grow and rearrange but don't form parallel layers, Example: quartzite and marble
Ways in which rocks are changed weathering, erosion, deposition, sediments, compaction, cementation, melting, cooling & hardening, heat & pressure
weathering process that breaks rocks into smaller pieces called sediments
erosion movement of weathered materials to new locations, where they are then deposited
deposition the laying down of rock forming material from any natural process
sediments small pieces of loose materials such as rock fragments, mineral grains, and bits of plant and animal remains
compaction occurs when small sediments stick together to form solid rock
cementation occurs when large sediments are glued together by minerals deposited between the sediments
melting when rocks are buried deep enough to be melted back into magma
cooling and hardening allows crystals to form
heat and pressure when existing rocks are buried deep and are heated by a nearby source of magma
Created by: user-1856292
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