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Published byLogan Benson Modified over 9 years ago
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The Rock Cycle The processes through which rocks are formed
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Igneous Rocks Form by the cooling of molten rock (either lava or magma) Typically have a texture of random crystals Form by the cooling of molten rock (either lava or magma) Typically have a texture of random crystals
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Iceland - 1980s, Alan Rubin
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Eruption of Mount St. Helens - May, 1980 (commercial slide)
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Mount St. Helens - 2004
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Middle and North Sister - Oregon Cascades
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Sedimentary Rocks Often form when particles weathered from earlier rocks are transported (by streams, wind or glaciers) and deposited as sediment The sediment is then buried and converted to rock by compression and cementation Typically have a texture of small rounded particles cemented together Often form when particles weathered from earlier rocks are transported (by streams, wind or glaciers) and deposited as sediment The sediment is then buried and converted to rock by compression and cementation Typically have a texture of small rounded particles cemented together
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French Pete Creek - Oregon Cascades
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Basin and Range - eastern Nevada
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Cochetopa Creek near Gunnison, Colorado
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Creek building delta into Lyman Lake - Washington Cascades
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Cape Cod, Massachusetts
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Canyonlands National Park, UT - Needles section
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Metamorphic Rocks Generally form when earlier rocks are subjected to high temperatures and/or pressures (BUT without melting!) Typically have a crystalline texture, with a pattern to the arrangement of crystals Generally form when earlier rocks are subjected to high temperatures and/or pressures (BUT without melting!) Typically have a crystalline texture, with a pattern to the arrangement of crystals
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Mt. Jefferson, Oregon Cascades
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http://www.personal.psu.edu/users/c/l/cll161/insys%20441/main.html
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