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PLATE TECTONICS. http://volcano.und.edu/vwdocs/vwlessons/plate_tectonics/introduction.html. Continental Crust. Cooling rate Crystal size Density Composition Thickness. http://www.amonline.net.au/geoscience/images/earth_diagrams/cont_oceanic_crust.gif. Oceanic Crust. Cooling rate
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PLATE TECTONICS http://volcano.und.edu/vwdocs/vwlessons/plate_tectonics/introduction.html
Continental Crust • Cooling rate • Crystal size • Density • Composition • Thickness http://www.amonline.net.au/geoscience/images/earth_diagrams/cont_oceanic_crust.gif
Oceanic Crust • Cooling rate • Crystal size • Density • Composition • Thickness http://faculty.weber.edu/bdattilo/parks/plume_ocean.jpg
Tectonic Plate • is a rigid piece of lithosphere floating on a partially plastic substrate (asthenosphere).
Pangea http://geology.csupomona.edu/drjessey/class/Gsc101/Plate.html
http://www.enchantedlearning.com/subjects/dinosaurs/glossary/Pangaea.shtmlhttp://www.enchantedlearning.com/subjects/dinosaurs/glossary/Pangaea.shtml
http://www.enchantedlearning.com/subjects/dinosaurs/glossary/Pangaea.shtmlhttp://www.enchantedlearning.com/subjects/dinosaurs/glossary/Pangaea.shtml
Evidence for Plate Tectonics • Continents ‘fit’ together
Evidence for Plate Tectonics • Continents ‘fit’ together • Fossil evidence
Evidence for Plate Tectonics • Continents fit together • Fossil distribution • Glacier evidence: deposits, striations
Evidence for Plate Tectonics • Continents fit together • Fossil distribution • Glacier evidence: deposits, striations • Climate distribution
Location of Trenches, Ridges, Mountains http://geology.csupomona.edu/drjessey/class/Gsc101/Plate.html
http://geology.csupomona.edu/drjessey/class/Gsc101/Plate.htmlhttp://geology.csupomona.edu/drjessey/class/Gsc101/Plate.html
Evidence for Plate Tectonics • Continents fit together • Fossil distribution • Glacier evidence: deposits, striations • Climate distribution • Location of mountain ridges, rifts, mid-ocean ridges, trenches
Magnetization http://www.ucmp.berkeley.edu/geology/tecmech.html
Evidence for Plate Tectonics • Continents fit together • Fossil distribution • Glacier evidence: deposits, striations • Climate distribution • Location of mountain ridges, rifts, mid-ocean ridges, trenches • Magnetic pattern of rock
Same Age Rocks http://geology.csupomona.edu/drjessey/class/Gsc101/Plate.html
Evidence for Plate Tectonics • Continents fit together • Fossil distribution • Glacier evidence: deposits, striations • Climate distribution • Location of mountain ridges, rifts, mid-ocean ridges, trenches • Magnetic pattern of rock • Common rock formations: same age
Volcano http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/GeoBytes%20GCSE%20Bl og%20Resources/Images/Plate%20Tectonics/Plate%20Tectonics/VolcanoStructure.jpg
Earthquake • http://news.bbc.co.uk/nol/shared/spl/hi/world/04/earthquake/img/earthquake.gif
Ring of Fire http://pubs.usgs.gov/gip/dynamic/understanding.html
Evidence for Plate Tectonics • Continents fit together • Fossil distribution • Glacier evidence: deposits, striations • Climate distribution • Location of mountain ridges, rifts, mid-ocean ridges, trenches • Common rock formations: same age • Magnetic pattern of rock • Location of earthquakes and volcanoes
Wegener’s Theory Problems • Continents plowing through the crust would destroy the crust • Continents are not moving apart at the speed Wegener proposed
Convection currents • Gravity causes the heated mantle to sink • The mantle heats up near the core and then rises again • Conduction is the transfer of heat between 2 materials in direct contact with each other library.thinkquest.org/C003124/images/convect.jpg http://www.wisc-online.com/objects/index_tj.asp?objID=SCE304 Click animation
Movement of mantle by convection allows melting and force to move plates
http://geology.csupomona.edu/drjessey/class/Gsc101/Plate.htmlhttp://geology.csupomona.edu/drjessey/class/Gsc101/Plate.html
Hot Spots – Hawaiian Islands http://geology.com/nsta/plate-tectonics-cover.gif