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Earth & Space Science Chapter 6

Earth & Space Science Chapter 6. Sedimentary and Metamorphic Rocks. Weathering vs. Erosion. Weathering: produces sediment by breaking down rock can be chemical or mechanical Erosion: t ransports sediment through moving water wind gravity Draw a picture of each

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Earth & Space Science Chapter 6

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  1. Earth & Space ScienceChapter 6 Sedimentary and Metamorphic Rocks

  2. Weathering vs. Erosion Weathering: • produces sediment by breaking down rock • can be chemical or mechanical Erosion: • transports sediment through • moving water • wind • gravity Draw a picture of each • glaciers of these factors.

  3. How can rocks form from sediment? • Lithification (lithos = stone): • Compaction—compression by overlying layers (sometimes pore space left, esp. sandstone) • Cementation—mineral “glue” • Sedimentary features • Bedding (seen in hwy rock cuts) • Ripple marks • Sorting/rounding of grains • Fossils

  4. Sedimentary Rock Features Bedding (horizontal layering):

  5. Sedimentary Rock Features • Most fossils are found in sedimentary rocks.

  6. Types of Sedimentary Rock Clastic—made of small bits (clasts) stuck together • Coarse (>2 mm pieces) • conglomerate • Medium (1/16 mm to 2 mm) • sandstone • Fine (1/256 mm to 1/16 mm) • siltstone • Very fine (< 1/256 mm) • shale

  7. Types of Sedimentary Rock Organic/Biochemical formed from/by living organisms • Coal • Fossiliferous limestone • Coquina • Chalk

  8. Types of Sedimentary Rock Chemical evaporites and precipitates • Rock salt • Rock Gypsum • Compact limestone • Chert/flint

  9. What causes metamorphism? • Temperature • Pressure

  10. Features of Metamorphic Rocks • Solid state change in minerals (remember Bowen’s reaction series?) • Foliation—parallel layers or bands—caused by pressure • Reorganization of crystals

  11. Protoliths of Foliated Rocks • Granite  gneiss (banded) • Various  schist (layered) • Shale  slate (layered)

  12. Protoliths of Nonfoliated Rocks • Limestone  marble • Sandstone  quartzite

  13. Types of Metamorphism • Low grade to high grade • Regional • Contact • Hydrothermal (hot groundwater)

  14. Economic Importance of Metamorphic Rocks • Building/Construction • Slate, marble • Metallic mineral resources • Ores (iron, lead) • Native minerals (gold, copper, silver) • Nonmetallic mineral resources • Talc, asbestos, graphite

  15. The Rock Cycle

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