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Types of Plate Boundaries

Types of Plate Boundaries. Created by Dr. Michael J. Passow. Wegener’s “Continental Drift”. Hypothesis: All continents once joined together as supercontinent PANGAEA. Over millions of years, continents split and moved to present positions (next slide)

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Types of Plate Boundaries

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  1. Types of Plate Boundaries Created by Dr. Michael J. Passow

  2. Wegener’s “Continental Drift” • Hypothesis: All continents once joined together as supercontinent PANGAEA. • Over millions of years, continents split and moved to present positions (next slide) • Evidence: matching coastlines, fossils, rocks, ancient climates • Weakness: no explanation of continents could move (“driving mechanism”) • Result: rejected for decades

  3. http://www.mapsharing.org/MS-maps/map-pages-worldmap/images-continental/1-continental-pangea-drift.gifhttp://www.mapsharing.org/MS-maps/map-pages-worldmap/images-continental/1-continental-pangea-drift.gif

  4. Emerging Evidence for Plate Tectonics • Mapping the ocean floors using echo-sounding (sonar) records • Paleomagnetism patterns in ocean basalt • Earthquake epicenter patterns • Volcano locations • Hot Spots (ex., Hawaii and the Emperor Seamounts) • Ocean drilling

  5. Continental Drift to Plate Tectonics By the late 1960s, the many lines of geoscience data obtained through developing technologies all provided evidence that: • 1) surface plates existed and • 2) they are moving very slowly in three basic patterns

  6. Divergent/Convergent/Transform plate boundaries http://www.uwsp.edu/gEo/faculty/ozsvath/images/plate_boundaries.htm

  7. Divergent Boundaries(spreading centers) http://www.geology110.com/files/lecshare1/html/web_data/file50.htm

  8. Continental Rift Valleys Perhaps the most famous example is the East African Rift Valley. Eventually, a new ocean may form here. (2- 3 million years ago, humans first evolved here.) http://education.usgs.gov/common/lessons/act5.html

  9. Convergent Boundaries(subduction zones) http://www.geology110.com/files/lecshare1/html/web_data/file51.htm

  10. Ocean-continent convergent boundaries http://sio.ucsd.edu/volcano/about/images/recycle.gif

  11. Most of the Pacific Ring of Fire consists of ocean-continent boundaries http://www.geocaching.com/seek/cache_details.aspx?guid=e83ed03c-349a-4ac5-a91c-a467cb9f92f2

  12. Ocean-ocean convergent boundary Japan http://blue.utb.edu/paullgj/physci1417/Lectures/Plate_Tectonics.html

  13. Continental-continentalconvergent boundary The Himalayas are one of the best examples of this type of boundary. http://www.utexas.edu/tmm/npl/mineralogy/mineral_genesis/index.html

  14. Transform Fault Boundaries http://www.geology110.com/files/lecshare1/html/web_data/file52.htm

  15. http://homepage.ufp.pt/biblioteca/GlossarySaltTectonics/Pages/PageT.htmlhttp://homepage.ufp.pt/biblioteca/GlossarySaltTectonics/Pages/PageT.html

  16. Continental transform fault:San Andreas system • Most transform faults exist in the ocean floor • One important exampleon a continent is the San Andrea system http://geology.com/articles/san-andreas-fault.shtml

  17. Putting It All Together http://www.geology110.com/files/lecshare1/html/web_data/file54.htm

  18. Causes (Driving Mechanisms) for Plate Tectonics • Convection • Slab-Pull and Ridge-Push • Mantle “plumes” • “Whole Mantle” and “Mantle-Core” models

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