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A mixture of minerals, volcanic glass, organic matter, or other material |
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A model showing processes that create and change rock. |
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Formed when sediments are pressed and cemented together. |
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Formed when a rock goes under extreme heat and pressure. |
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Formed for the cooling and hardening of magma or lava. |
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The rock cycle never destroys elements of rock but merely redistributes them. |
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The father of the rock cycle. |
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Magma from a volcano that reaches Earth's surface. |
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Large-grained igneous rock forms when magma cools below the surface. |
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Small-grained igneous rock forms when magma cools at or near the Earth's surface. |
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dark-colored and dense igneous rock that is mostly likely to be found near the ocean floor. |
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Contain Fe and Mg but very little silica |
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Lower in density and lighter in color |
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Contains more silica and less Fe and Mg |
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Balanced composition of minerals and density |
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can help identify and igneous rock as intrusive or extrusive |
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Igenous rock with holes around once trapped air and other gases |
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Basaltic, granitic and andesitic |
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Two ways that igneous rocks are classified |
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Change from the heat and pressure caused by one layer rock on top of another rock. |
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Can change as a result of hot, water-rich fluids moving through rock, chemically changing it. |
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Two ways to classify metamorphic rocks |
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classified by the composition and texture |
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Mineral grains flatten and line up in parallel layers of bands |
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Mineral grains grow and rearrange but do not form layers |
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Mostly found exposed on Earth's surface |
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Layers of rocks, fragments, mineral grains, organic matters |
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Classified by what they are made of and how they are formed. |
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Occurs when small sediments stick together because of pressure |
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Occurs when water and other minerals move through open spaces between larger sediments gluing them together |
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Detrital Sedimentary Rocks |
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Made from broken fragments of other rocks and often have a granular texture |
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Chemical Sedimentary Rock |
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Limestone and rock salt are two examples |
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Forms from calcite, which was calcium carbonate in solution |
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Formed from halite, which was salt in solution |
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Made from remains of once-living plants or animals |
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Made of microscopic calcite-shell remains of animals |
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Made of plant remains, chemically changed by microorganisms and compacted over million of years |
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