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Rocks
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Different from minerals
Can be organic Classified by: Color Texture Mineral composition Origin (how they were formed). Three main groups of rocks.
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Igneous Rocks Formed by cooled magma or lava.
Found in volcanic regions 2 types: Intrusive: Rocks that cool under Earth’s surface. Cool slowly. Grains of rock are bigger Extrusive: Rocks that cool on Earth’s surface. Cool quickly. Grains of rock are smaller, with more air spaces (pores)
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Examples Intrusive rocks: Extrusive rocks: Granite Basalt - Obsidian
- Pumice
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Sedimentary Rocks 5 step process creates sedimentary rocks Deposition:
Sediments are laid down in a new location. Build up in layers. Weathering: Existing rock is broken down into sediments. Erosion: Sediments are carried away to a new location Cementation: Sediments are glued together by a chemical reaction. Compaction: Sediments are pressed together by the wieght of new sediment on top.
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Sedimentary Rocks cont.
Usually seen in layers. Fossils are found only in sedimentary rocks.
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Examples Sandstone Shale Limestone Conglomerate
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Metamorphic Rocks Formed by heat and pressure acting on existing rocks. (heat & pressure) Sandstone Quartzite
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Other Examples (heat & pressure) Shale Slate (heat & pressure) Granite
Gneiss
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(heat & pressure) Limestone Marble
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Metamorphic rocks cont.
2 types: Foliated: The grains of the rocks are arranged in parallel layers or bands. Nonfoliated: Grains are not arranged in parallel layers.
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