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rocks
| Question | Answer |
|---|---|
| Rocks: | Rocks: Make up the earth's crust, that are made of a mixture of minerals and other materials |
| 2. Classifying Rocks: | 2. Classifying Rocks: 3 ways of classifying |
| A. Texture: | A. Texture: the look and feel of the rocks surface; the grain: what gives the rock its texture. |
| 1. Grain size 2. Grain shape 3. Grain pattern 4. No visible grain | 1. Grain size 2. Grain shape 3. Grain pattern 4. No visible grain |
| B. Mineral Composition: | B. Mineral Composition: geologists use a microscope to observe the shape and size of the rock’s crystals. |
| C. Origin: | C. Origin: 1. Sedimentary: forms in layers 2. Igneous: forms from magma or lava 3. Metamorphic: formed deep underground |
| 1. Igneous Rocks Classified: | 1. Igneous Rocks Classified: formed from intense heat that comes from magma or lava. |
| A. Extrusive Rocks: | A. Extrusive Rocks: igneous rocks formed from lava that erupted onto Earth's surface |
| B. Intrusive Rocks: | B. Intrusive Rocks: igneous rocks formed from magma that hardens beneath Earth's surface. |
| C. Texture: | C. Texture: depends upon the size and shape of the crystals |
| 1. Porphyritic texture: | 1. Porphyritic texture: large crystals surrounded by small crystals, which form when magma cools in two stages. |
| 2. Uses of Igneous Rocks: | Basalt: gravel Pumice: cleaning and polishing Perlite: soil mixes Obsidian: sharp tools Granite: building materials |
| Sedimentary | Sedimentary Rocks: formed from layers of sediment deposited by water and wind; |
| 2. Changing sediments to rocks: | A. Erosion: wind or water carry sediments B. Deposition: when the water or wind stops carrying the sediments C. Compaction: presses sediments together D. Cementation: when dissolved minerals and sediment glue together. |
| Clastic Rocks: | Clastic Rocks: formed sedimentary rocks are squeezed together |
| 1. Examples of clastic rocks: | 1. Examples of clastic rocks: shale, sandstone, conglomerate, and breccia |
| Organic Rocks: | Organic Rocks: formed when layers of plants and animals are deposited in thick layers |
| 1. Examples of organic rocks: | 1. Examples of organic rocks: coal, and limestone |
| chemical Rocks: | chemical Rocks: when minerals are dissolved in a solution crystallize |
| Uses of Sedimentary Rocks: | Uses of Sedimentary Rocks: A. Limestone and sandstone: building materials B. Coal: fossil fuel |
| . Metamorphic Rocks: | . Metamorphic Rocks: formed from heat and pressure deep beneath the earth's surface change sedimentary and igneous rocks into metamorphic |
| Grains: | Grains: the arrangement of the grains |
| foliated: | foliated: grains arranged in parallel layers or bands |
| Non-foliated: | Non-foliated: mineral grains are arranged randomly |
| 2. Uses of Metamorphic Rocks: | 2. Uses of Metamorphic Rocks A. Marble: building materials B. Slate: flooring, roofing, chalkboards |
| Limestone | Limestone changes to marble |
| B. Sandstone | B. Sandstone changes to quartzite |
| C. Shale | C. Shale changes to slate |
| D. Granite | D. Granite changes to gneiss |
| . The Rock Cycle: | . The Rock Cycle: Forces inside the Earth and at the surface of the Earth produce a rock cycle that builds, destroys, and changes the rocks in the crust. |
| A. Sub-ducting Oceanic Plates: | A. Sub-ducting Oceanic Plates: Plate movements (downward) drive the rock cycle by pushing rocks back into the mantle, where they melt and become magma again. |
| Colliding Continental Plates: | Colliding Continental Plates: Plate movement that causes folds, faulting, and uplifting of the crust that move rocks through the rock cycle. |
| 2. Grain shape | 2. Grain shape |
| 3. Metamorphic: formed deep underground | 3. Metamorphic: formed deep underground |
| 1. Sedimentary: | 1. Sedimentary: forms in layers |
| 2. Igneous: forms from magma or lava | 2. Igneous: forms from magma or lava |