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Ch.3 The Rock Cycle
| Term | Definition |
|---|---|
| Rock | Any solid mass of mineral or mineral like matter that occurs naturally as part of our planet. |
| Igneous Rock | A rock formed by the crystallization of molten magma. |
| Sedimentary Rock | Rock formed from the weathered products of preexisting rocks that have been transported, deposited, compacted, and cemented. |
| Metamorphic Rock | Rock formed by the alteration of preexisting rock deep within Earth (but still in the solid state) by heat, pressure, and/or chemically active fluid. |
| Rock Cycle | The continuous processes that cause rocks to change. |
| Magma | Molten material that forms deep beneath Earth's surface. |
| Lava | Magma that reaches the surface. |
| Weathering | A process in which rocks are physically and chemically broken down by water, air, and living things. |
| Sediments | Weathered pieces of Earth materials. |
| Intrusive Igneous Rocks | Rocks that form when magma hardens beneath Earth's surface. |
| Extrusive Igneous Rocks | Rocks that form when lava hardens. |
| Porphyritic Texture | Rocks wirth very different size minerals and experience different rates of cooling. |
| Granitic Composition | Igneous rocks with the main minerals being quartz and feldspar. |
| Basaltic Composition | Rocks that contain many dark silicate minerals and plagioclase feldspar. |
| Andesitic Composition | Rocks with a composition between granitic and basaltic rocks. |
| Erosion | Weathering and the removal of rock. |
| Deposition | When an agent of erosion (water, wind, ice, or gravity) loses energy and drops the sediments. |
| Compaction | A process that squeezes, or compacts, sediments. |
| Cementation | When dissolved minerals are deposited in the tiny spaces among the sediments. |
| Clastic Sedimentary Rocks | Sedimentary rocks that are made of weathered bits of rocks and minerals. |