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Published byMadelynn Simon Modified over 10 years ago
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Coach Williams Room 310B
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Formation of Sedimentary Rocks
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Formed by cemented sediments
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Solid material Deposited on Earth’s surface Wind, water, ice, gravity, chemical precipitation Form sedimentary rocks
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Earth’s crust is worn down Physical or chemical processes Clastic sediments- rock or mineral fragments ◦ Greek klastos = broken
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Removal and movement of rock fragments 4 Main ways: ◦ Wind ◦ Moving water ◦ Gravity ◦ Glaciers Deposition- sediments laid down ◦ Land and water http://www.youtube.com/watch?v=51C7vEAVbxk http://www.youtube.com/watch?v=51C7vEAVbxk
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Sediments become rock Greek lithos = rock Layers of sediment = pressure Deep layers = hot temperature Cementation- mineral growth cements sediment together
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Bedding- horizontal layering Graded Bedding- larger/heavier fragments at bottom layers Cross-Bedding- layer crossing over another one
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Preserved evidence of once-living organisms ◦ Remains or impressions Found in sedimentary rocks
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Types of Sedimentary Rocks
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Clastic- deposited loose fragments Chemical- dissolved minerals left behind
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Classified by sediment size Coarse-grained: gravel-sized fragments Medium-grained: sand-sized fragments Fine-grained: silt-sized fragments Porosity- % of open spaces
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Evaporation- leaves minerals behind ◦ Evaporites: rocks formed this way Organic- remains of once-living organisms ◦ Shells, bones ◦ Coal- remains of plant material; carbon; fuel
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Energy- coal, natural gas, oil, nuclear Fertilizers Iron Walls/buildings Snapshot- cross bedding & fossils
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http://geology.com/rocks/sedimentary-rocks.shtml http://geology.com/rocks/sedimentary-rocks.shtml
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Metamorphic Rocks
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Temperature/pressure changes rocks ◦ Composition, minerals, texture Meta = change Morph = form
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Regional: large regions Contact: molten rock touches solid rock Hydrothermal: hot water alters rock
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Foliated: minerals are wavy layers/bands Non-foliated: no mineral grains in one directions
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http://geology.com/rocks/metamorphic-rocks.shtml http://geology.com/rocks/metamorphic-rocks.shtml
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Changing and re-making of rocks
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