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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
– Chocolate: when it’s cold, it’s hard and breaks, but as it warms up it can bend and eventually melt
• Asthenosphere– Honey: it’s thick and sticky, but it flows
• Mantle– Crumbled cookies: it’s solid but can move and
convect
• Outer core– Milk: liquid
• Inner core– Peach pit: solid
Plate Boundaries
Stern, R. J., Subduction zones, Rev. Geophys., 40(4), 1012, doi:10.1029/2001RG000108, 2002
Margins: Divergent• Mid-Ocean Ridges
– Mid Atlantic Ridge
• Continental Rifts– East African Rift Valley
http://www.phschool.com/atschool/phsciexp/internet_activity/cfd-1014_midocean.html
http://www.talktalk.co.uk/reference/encyclopaedia/hutchinson/m0006339.html
Margins: Convergent
• Ocean-ocean subduction– Island arc: Marianas
http://www.see.leeds.ac.uk/structure/dynamicearth/subduction/cordillera_islandarc.htm
Margins: Convergent
• Ocean-continent subduction– Volcanic arc and mountains: Andes
http://www.see.leeds.ac.uk/structure/dynamicearth/subduction/cordillera_islandarc.htm
Margins: Convergent
• Continent-continent collision– Large mountain range: Himalayas and Alps
http://www.unil.ch/igp/page23575_en.html
Margins: Transform• Marine
– Transform faults: • Mid Atlantic Ridge
• Terrestrial– Strike-slip faults:
• San Andreas Fault
http://geomaps.wr.usgs.gov/archive/socal/geology/inland_empire/socal_faults.html
Evidence for Plate Tectonics• Fit of the continents• Sea floor ages and magnetic anomalies –
evidence of ocean spreading• Paleontology – similar species on now widely
separated continents• Seismicity and volcanism concentrated at
plate boundaries – evidence of oceanic subduction
• Hot spot tracks – record movement of plates over “fixed” hot spot
• GPS