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Minerals and Rocks
Vocabulary
| Term | Definition |
|---|---|
| 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 |