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Age of the Earth
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Subdivisions of geologic time –Eon, Era, Period, Epoch –Eons Precambrian: 4.5 b.y. to ~0.5 b.y. Phanerozoic: ~0.5 b.y. to today Geologic time scale
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Subdivisions of geologic time –Eon, Era, Period, Epoch –Eras Paleozoic: ~560 m.y. to ~250 m.y. Mesozoic: ~250 m.y. to ~65 m.y. Cenozoic: ~65 m.y. to today Geologic time scale
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Image source: http://www.gly.fsu.edu/~salters/GLY1000/12Rock_record_time/Slide27.jpg
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Plate Tectonics- Overview Plate Tectonics–General Principles Plate Movements–Accumulating Evidence Types of Plate Boundaries How Far, How Fast, How Long, How Come? Plate Tectonics and the Rock Cycle
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Plate Tectonics–General Principles Stress and Strain in Geologic Materials Lithosphere and Asthenosphere Locating Plate Boundaries
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Tectonics Stress- application of a force –Compressive (pushing together) –Tensile (pulling apart) Strain- deformation response of the force –Elastic deformation: ‘rubber band’ –Plastic deformation: permanent strain –Rupture: the breaking point
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Folding Rock Source: Photograph courtesy of M.R. Mudge; courtesy USGS Photo Library, Denver, CO.
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Folding and Faulting, Cook Inlet, Alaska Source: Photograph by N.J. Silberling, USGS Photo Library, Denver, CO.
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Rock Failure Under Stress Source: Photograph courtesy of W.B. Hamilton; courtesy USGS Photo Library, Denver, CO.
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Effect of tectonics on rocks Depends of physical conditions –Temperature & pressure –composition, time, fluids
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Lithosphere- Asthenosphere
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Lithosphere-Asthenosphere Lithosphere (lithos = rock) –Brittle, elastic outer layer –~50 km under oceans, ~100 km under continents Asthenosphere (asthenes= without strength) –Plastic domain –~300 km in mantle –Discovered by seismic wave studies
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Plate boundaries Deformation, earthquakes, and volcanoes are not evenly distributed around the Earth Mostly concentrated in linear belts, chains Can use distribution to ‘map out’ plates ~8 major plates, several smaller ones
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World Locations of Volcanoes and Earthquakes Source: Map plotted by the Environmental Data and Information Service of NOAA; earthquakes from U.S. Coast and Geodetic Survey.
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Plate Movements–Accumulating Evidence The Topography of the Sea Floor Magnetism in Rocks–General Paleomagnetism and Seafloor Spreading Age of the Ocean Floor Polar-Wander Curves Other Evidence
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Shaded Relief Map of the World Source: Photo courtesy of NOAA National Geophysical Data Center.
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Shaded Relief Map of the World Source: Photo courtesy of NOAA National Geophysical Data Center.
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The Earth is a large bar magnet… And sometime it flips…!
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(1) Minerals oriented randomly in a melt (2) Minerals aligned in the magnetic field Minerals: the ‘Curie Temperature’
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First magnetic survey of the oceans
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Age Distribution of the Sea Floor Source: Marine Geology and Geophysics Division of the NOAA National Geophysical Data Center.
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World Locations of Volcanoes and Earthquakes Source: Map plotted by the Environmental Data and Information Service of NOAA; earthquakes from U.S. Coast and Geodetic Survey.
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World Lithospheric Plates Source: After W. Hamilton, U.S. Geological Survey.
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Source: http://www.mq.edu.au/scienceresearch/lackie.htm Polar Wander
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Plate Movements — Today Source: After R.S. Dietz and J.C. Holden, “Reconstruction of Pangaea,” Journal of Geophysical Research, 75:4939-4956, 1970, copyright by the American Geophysical Union.
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Plate Movements — 100 Million Years Ago Source: After R.S. Dietz and J.C. Holden, “Reconstruction of Pangaea,” Journal of Geophysical Research, 75:4939-4956, 1970, copyright by the American Geophysical Union.
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Plate Movements— 200 Million Years Ago Source: After R.S. Dietz and J.C. Holden, “Reconstruction of Pangaea,” Journal of Geophysical Research, 75:4939-4956, 1970, copyright by the American Geophysical Union.
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Glacial Deposits Across Southern Continents Source: After Arthur Holmes, Principles of Physical Geology, 2d ed., Ronald Press, New York, NY, 1965.
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Types of Plate Boundaries Divergent Plate Boundaries –Rifts, Mid ocean ridges, lots of volcanism Transform Boundaries –Sliding plates, lots of earthquakes Convergent Plate Boundaries –Subduction zones, mountain belts
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Divergent plate boundary: East African Rift
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Satellite Image of Lake Tanganyika, Africa Source: © NASA
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Transform plate boundary: San Andreas strike-slip fault
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Convergent plate boundary: Subduction Zone in Alaska Source: Image courtesy of NOAA National Geophysical Data Center.
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Convergent plate boundary: Where are we?
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Current Motions of Major Plates: Satellite laser data Source: Data from NASA.
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