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Published byMaximilian Pillman Modified over 9 years ago
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Some Basic Geology Classes of Rocks
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Igneous Formed by solidification of gaseous or molten material from cooling magma or lava More commonly seen in areas such as the Canadian Shield where bedrock from the Precambrian lies at the surface. Examples: basalt, obsidian, granite (cools more slowly), volcanic ash (tuffa, pumice)
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Basalt
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Basalt Columns Giant's Causeway - Ireland
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Devil’s Tower, WY
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Basalt Columns Keweenaw Peninsula Michigan
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Basalt with Opal
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Obsidian
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Obsidian
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Obsidian
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Granite
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Volcanic Ash (Tuff)
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Volcanic Ash (Pumice)
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Canadian Shield
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Sedimentary Formed by compaction of material Clastic rocks: older rock broken up by ice, wind, water (erosion) Shale, sandstone, clay Organically/chemically produced rocks Limestone, chalk, coal – from living organisms Salt - chemical Gypsum - chemical
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Limestone
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Starfish in Illinois limestone
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Thornton Quarry
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Layers of sediment formed on a sloping portion of the Silurian reef.
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Devonian Dolomite Silurian Limestone: which is older?
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Dolomite from Joliet Dolomite cliff
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Sandstone
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Saint Peter Sandstone along Rock River
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French Canyon at Starved Rock State Park. Also St. Peter sandstone.
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Pictured Rocks National Lakeshore, Michigan Lake Superior
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Puddingstone Type of sedimentary rock Michigan Puddingstone is a conglomerate of primarily quartzite and pebbles of jasper
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Metamorphic Form when igneous or sedimentary rocks are changed by heat, pressure, or infiltration with other materials Characteristics flaky: slate (comes from mud) non-flaky: marble (comes from limestone) sparkly: gneiss (comes from igneous or sedimentary rocks) Quartzite: comes from sandstone
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Slate – metamorphic mud
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Marble – metamorphic limestone
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Metamorphic Granite Gneiss = sparkling
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Quartzite – Metamorphic sandstone
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Baraboo Quartzite, Wisconsin
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