plate tectonics

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Plate Tectonics. A Brief Overview. The Earth ’ s Plates. http://www.nature.nps.gov/geology/usgsnps/pltec/pltec2.html. Layers of the Earth. Chemical. Physical. http://www.burkemuseum.org/static/geo_history_wa/The%20Restless%20Earth%20v.2.0.htm. Layers of the Earth and Food. Lithosphere - PowerPoint PPT Presentation

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  • Plate TectonicsA Brief Overview

  • The Earths Plateshttp://www.nature.nps.gov/geology/usgsnps/pltec/pltec2.html

  • Layers of the EarthChemicalPhysicalhttp://www.burkemuseum.org/static/geo_history_wa/The%20Restless%20Earth%20v.2.0.htm

  • Layers of the Earth and FoodLithosphereChocolate: when its cold, its hard and breaks, but as it warms up it can bend and eventually meltAsthenosphereHoney: its thick and sticky, but it flowsMantleCrumbled cookies: its solid but can move and convectOuter coreMilk: liquidInner corePeach pit: solid

  • Plate BoundariesStern, R. J., Subduction zones, Rev. Geophys., 40(4), 1012, doi:10.1029/2001RG000108, 2002

  • Margins: DivergentMid-Ocean RidgesMid Atlantic RidgeContinental RiftsEast African Rift Valleyhttp://www.phschool.com/atschool/phsciexp/internet_activity/cfd-1014_midocean.htmlhttp://www.talktalk.co.uk/reference/encyclopaedia/hutchinson/m0006339.html

  • Margins: ConvergentOcean-ocean subductionIsland arc: Marianashttp://www.see.leeds.ac.uk/structure/dynamicearth/subduction/cordillera_islandarc.htm

  • Margins: ConvergentOcean-continent subductionVolcanic arc and mountains: Andeshttp://www.see.leeds.ac.uk/structure/dynamicearth/subduction/cordillera_islandarc.htm

  • Margins: ConvergentContinent-continent collisionLarge mountain range: Himalayas and Alpshttp://www.unil.ch/igp/page23575_en.html

  • Margins: TransformMarineTransform faults: Mid Atlantic RidgeTerrestrialStrike-slip faults: San Andreas Faulthttp://geomaps.wr.usgs.gov/archive/socal/geology/inland_empire/socal_faults.html

  • Evidence for Plate TectonicsFit of the continentsSea floor ages and magnetic anomalies evidence of ocean spreadingPaleontology similar species on now widely separated continentsSeismicity and volcanism concentrated at plate boundaries evidence of oceanic subductionHot spot tracks record movement of plates over fixed hot spotGPS