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Appalachian Mountain Building

Appalachian Mountain Building. Chapter 20 Section 2 Lauren Bauschard Jamie Reed. Orogeny. Orogeny is the process that for all mountain ranges. Orogeny results in broad, linear regions of deformation known as orogenic belts. Most orogenic belts are associated with plate boundaries.

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Appalachian Mountain Building

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  1. Appalachian Mountain Building Chapter 20 Section 2 Lauren Bauschard Jamie Reed

  2. Orogeny • Orogeny is the process that for all mountain ranges. • Orogeny results in broad, linear regions of deformation known as orogenic belts. • Most orogenic belts are associated with plate boundaries. • The greatest variety and the tallest of these belts Are found at convergent Boundaries.

  3. Oceanic-Oceanic Convergence • When an oceanic plate converges with another oceanic plate, one plate descends into the mantle to create a subduction zone. • As parts of the subducted plate melt, magma is forced upward to form a series of volcanic peaks called an island arc complex.

  4. Oceanic- Continental Convergence • Same as O-O boundaries in that convergence along both creates subduction zones and trenches. • Convergence between O-C plates can produce major mountain belts • The descending oceanic plate forces the edge of the continental plate upwards. This uplift marks the beginning of orogeny. • In addition to uplift, compressive forces may cause the continental crust to fold and thicken.

  5. Oceanic-Continental Convergence

  6. Continental-Continental Convergence • Continental crust cannot be subducted into the mantle when two plates converge because of its relatively low density. • Instead, the energy associated with the collision is transferred to the crust involved, which becomes highly folded and faulted.

  7. Continental-Continental

  8. The Early Appalachians • Tectonic history of the Appalachian Mountains started about 700 to 800 years ago. • Ancestral North America separated from ancestral Africa along two divergent boundaries to form two oceans • A continental fragment was located between the two divergent boundaries.

  9. 700-600 M.Y.B.P • During this time the directions of plate motions reversed. • The ancestral Atlantic Ocean began to close as the plates converged. • This convergence resulted in the formation of a subduction zone and a volcanic island arc east of ancestral North America.

  10. 700-600 M.Y.B.P

  11. 500-400 M.Y.P.B. • At this time the continental fragment became attached to ancestral North America. • The highlt metamorphosed rocks, were thrust over younger rocks to become the Blue Ridge Province.

  12. 500-400 M.Y.B.P.

  13. 400-300 M.Y.B.P. • At this time the island arc became attached to North America. • This is proved in the Piedmont Province. • These rocks were also faulted over the continent pushing the Blue Ridge rocks farther west.

  14. 400-300 M.Y.B.P.

  15. 300-260 M.Y.B.P. • During this time the ancestral Atlantic Ocean closed as ancestral Africa, Europe, and South America collided with ancestral North America to form Pangaea. • This is when the modern Atlantic Ocean formed.

  16. 300-260 M.Y.B.P.

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