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Conversations with the Earth Tom Burbine tburbine@framingham.edu

Conversations with the Earth Tom Burbine tburbine@framingham.edu

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Conversations with the Earth Tom Burbine tburbine@framingham.edu

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  1. Conversations with the EarthTom Burbinetburbine@framingham.edu

  2. Next week • No class

  3. Midterm • March 24 • You can bring in a sheet of paper with anything written on it • You can bring in your hand-written mineral sheets

  4. Rocks on the Surface • If you can see rocks on the surface that comes from the interior, you can study them

  5. Rocks can deform and flow • Easier for rock to deform and flow when it is warmer

  6. Lithosphere • Lithosphere is a planet’s outer layer of cool and relatively rigid rock • Asthenosphere is the region in the upper mantle characterized by low-density, semiplastic (or partially molten) rock material chemically similar to the overlying lithosphere

  7. Heating of Planet

  8. How does the planetary interior cool off? • Heat is transported outward

  9. How does the planetary interior cool off?

  10. Plate Tectonics • Plate tectonics describes the large scale motions of Earth's lithosphere.

  11. Pangea • Pangea - One large supercontinent http://geology.csupomona.edu/drjessey/class/Gsc101/pangea.gif

  12. Principles of Plate Tectonics • 1. The surface of the Earth is composed of lithospheric plates that are in constant motion. • The plates move in response to plastic flow in the athenosphere. • Motion in the asthenosphere is caused by convection driven by the Earth’s internal heat. • The internal heat comes from radioactive decay and the latent heat from the Earth’s formation.

  13. Three Types of Plate Tectonic Boundaries • Divergent – plates move apart, space is filled with molten magma • Convergent – plates collide • Transform – plates slide horizontally past each other

  14. Divergent plate boundary

  15. Convergent Plate Boundary

  16. Hot spots

  17. Transform Boundaries

  18. Any Questions?