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Published byTerence Cole Modified over 9 years ago
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Earth Science A study in Change: Rocks Watch for & It will tell you when/where information will be used in this unit!
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Rocks Any sold mass of minerals, or mineral like material. Inorganic solid, crystalline structure, definite chemical composition. Isn’t a rock, just a rock? So what? They aren’t static objects. They change with the earth and can tell us about it. Their timeline is just different than ours!
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Most Common Minerals (pg 35) Know these!
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Main Types of Rock Igneous Sedimentary Metamorphic Processes that change rock Melting & cooling Weathering & erosion Compaction & cementation Heat & Pressure
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Igneous Rocks Form from the cooling of magma or lava. Magma = molten rock below the surface of the earth (625 o C or 1032 o F, low end) Intrusive igneous rock Composed of silicon, oxygen, & gases like water vapor Lava = molten rock above the surface of the earth Extrusive igneous rock Similar in composition to intrusive igneous, without the gases (low pressure = escape)
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Igneous Characteristics Texture Course grained - large crystals caused by slow cooling of magma, usually intrusive Fine grained - small interlocking crystals due to relatively fast cooling Glassy - cools too quickly to form crystals, may appear glassy, may not (obsidian vs. pumice)pumice Porphyritic - both large and small crystals due to varying rates of cooling
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Igneous Characteristics Composition Granitic - made up of mostly quartz or feldspar Tend to be light colored Basaltic- made up of mostly dark silicates, rich in magnesium and iron Tend to be dark colored Other - either a combination of the above or ultramafic (really old rocks)
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Igneous Rock Examples Obsidian Lava flow= basaltGranite AphaniticPorphyritic
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Sedimentary Rocks Form when existing rocks are broken down into sediments and the sediments are cemented together to form a “new” (recycled) rock. Weathering - process by which existing rock is broken down. Physical weathering - breaking of a large rock into smaller pieces(physical changes) Chemical weathering - changing of rock composition due to chemical changes
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Processes Forming Sedimentary Rocks Weathering Ice wedging, root action, acid rain Faster when there is lots of water in environment Erosion - process by which weathered sediment is transported away from original parent rock. Wind, Water, Ice, Gravity Deposition - fancy term for when the eroded particles are dropped!
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Processes Forming Sedimentary Rocks Compaction - process of squeezing or smashing of deposited sediments into a smaller volume Usually due to the weight of new sediments being deposited above. Cementation - process of gluing sediments together Dissolved minerals precipitate out of solution and are deposited in the space between sediments.
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Classification of Sedimentary Rocks Clastic Sedimentary- composed of weathered sediments and minerals Conglomerate, sandstone, shale Bits and pieces stuck together. Looks or feels chunky Chemical Sedimentary - composed from precipitates of dissolved minerals Limestone, rock salt, gypsum(drywall)
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Sedimentary Rock Examples Sandstone- Clastic Limestone -Chemical Conglomerate - Clastic
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Metamorphic Rock Formed when existing rocks are changed by heat and pressure(causes chemical reactions). Heat - provides energy for chemical reactions Earth structure provides heat source Amount required to change a rock depends upon its mineral composition Chemical Reactions - hot water containing other substances that allow recrystallization Pressure - from all directions, affected by depth
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Types of metamorphic rock Foliated - layered or banded appearance of metamorphic rocks Due to parallel orientation of mineral crystals Forms when sedimentary rock is smashed Nonfoliated - does not have banded texture, usually made up of only one mineral.
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Metamorphic Rock examples Sandstone, before/after, nonfoliated Slate (parent = shale) foliated
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Metamorphic Examples Marble nonfoliated Quartzite nonfoliated
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Rock Cycle (final exam)
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