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