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Published byCuthbert Edwards Modified over 9 years ago
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Types of Rocks
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3 Basic Types Sedimentary Igneous Metamorphic
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3 Types of Sedimentary Rocks Clastic Chemical Organic
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Clastic Sedimentary Rock Sediments form when rocks are weathered and eroded Sediments are moved by wind, glaciers and water Most clastic sediments are deposited in the ocean
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Clastic Sedimentary Rock Particle size is key to type of rock –Gravel is > 2 mm –Sand is 1/16 mm to 2 mm –Mud is < 1/16 mm Clay is < 4 um Silt is > 4 um
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Sandstone
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Conglomerate
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Shale
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Chemically Precipitated Sedimentary Rock Ions released during chemical weathering are carried away in solution Inorganic Precipitates –Halite –Gypsum Organic precipitates –Silica (diatoms) –Calcium carbonate – shells - CaCO 3 –Dolomite - CaMg(CO 3 ) 2
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Halite
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Gypsum
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Diatomaceous Earth
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Limestone
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Dolomite
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Organic Sedimentary Rock Sediments or rocks consisting mostly or entirely from plant material –Peat –Coal BituminousAnthracite
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Sedimentary Environments Lakes Lower courses of rivers Shallow ocean Deep ocean
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Extrusive & Intrusive Igneous Rocks Intrusive- Magma under the surface –Coarse-grained –Magma cools slowly and large crystals grow over a long period of time –Gabbro, diorite, granite
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Granite
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Gabbro
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Extrusive & Intrusive Igneous Rocks Extrusive- Lava at the surface –Fine-grained –Lava cools very quickly, consequently crystals do not have time to grow and develop –Basalt, andesite, rhyolite, obsidian
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Basalt
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Rhyolite
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Obsidian
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Explosive Volcanism Fragmented magma ejected explosively –Ash plumes –Pyroclastic flows
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Pumice
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Metamorphic Rocks Rocks change at the chemical level Grade of metamorphism Shearing Foliation
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Nature of Metamorphism Changes take place while a solid Due to heat and pressure Protolith – original rock
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Metamorphic Rocks Foliated vs. Nonfoliated
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Metamorphic Rocks Foliated- Metamorphic rock in which minerals have been rearranged into visible bands.
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Schist
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Gneiss
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Slate
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Metamorphic Rocks Nonfoliated- Metamorphic rock that does not show bands.
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Marble
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Quartzite
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Regional vs. Contact Metamorphism Regional Contact (or thermal)
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Contact Metamorphism
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