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Published byAngela Brummitt Modified over 9 years ago
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Plate Tectonics
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Major Divisions of Earth Plate Tectonics
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Different Properties Plate Tectonics
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Rigid Plate Tectonics Plastic
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The outer layer is the thinnest = Crust Two kinds of Crust Plate Tectonics
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continental crust : thicker, light (granite) oceanic : thinner, dense (basalt) Plate Tectonics 2.7g/cm³ 3.3 g/cm³
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Each Tectonic Plate: Oceanic crust or Oceanic & Continental crust Plate Tectonics
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Each Tectonic Plate: Oceanic crust or Oceanic & Continental crust (none with continent only) Plate Tectonics
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Oceanic crust or Oceanic & Continental crust Plate Tectonics
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Active continental margin: leading edge of plate (earthquakes, volcanoes, steep mountains) Plate Tectonics
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Passive continental margin: trailing edge of continent (eroded mountains, flat plains, little activity) Plate Tectonics
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http://www.simonwinchester.com/images/map1_large.jpg
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Active margin Passive margin
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Plate Tectonics Classification of Plate Boundaries
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Plate Tectonics I. Divergent Boundaries : tension = pull apart normal faults
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Plate Tectonics I. Divergent Boundaries : tension = pull apart normal faults http://web.mala.bc.ca/earle/geol201/rift-valley2.gif
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Plate Tectonics I. Divergent Boundaries : new ocean crust formed mid-ocean ridge with a rift valley down the middle
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Plate Tectonics I. Divergent Boundaries : young basin
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Plate Tectonics I. Divergent Boundaries : mature basin
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Plate Tectonics I.Convergent Boundaries : compression = push together reverse faults
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Plate Tectonics I.Convergent Boundaries : compression = push together reverse faults http://geology.wr.usgs.gov/parks/deform/hangfootwall.gif
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Plate Tectonics I.Convergent Boundaries : folding & uplift earthquakes http://geology.wr.usgs.gov/parks/deform/hangfootwall.gif
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Plate Tectonics Three kinds of Convergent Margins (Crust Type) oc - oc oc - cont. cont. - cont.
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Plate Tectonics IIa. Ocean - Ocean deep sea trench subduction zone (recyle) volcanoes & uplift
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Aleutians, Japan, Philippines, Indonesia
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Plate Tectonics IIb. Ocean - Continent deep sea trench subduction zone (recycle ocean side) volcanoes & major uplift
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Plate Tectonics IIb. Ocean - Continent
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Andes, Cascades
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Plate Tectonics IIc. Continent - Continent collision no subduction, no vulconism (can't recyle continents) heat & pressure, folding & major uplift
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Plate Tectonics IIc. Continent - Continent
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Himalayas
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Plate Tectonics III. Transform Plate boundaries shear = sliding past in opposite directions lateral movement with earthquakes
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Plate Tectonics III. Transform Plate boundaries California San Andreas fault
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