Plate Tectonics: The Grand Unifying Theory of Geology

More documents

Recommendations

Info

Type 1 - Divergent Plate Boundary • Divergent - Two plates that pull away or separate from each other. • Produce new crust • Examples: Mid Atlantic Ridge, East Pacific Rise • Effect of movement – Sea Floor Spreading :: Divergent Animation ::
Type 2 - Convergent Plate Boundary • Convergent - Two plates that move towards or collide with each other. • Consume old crust • Example, India into Asia, NW Coast of U.S. SW coast of South America • Effect of movement – Subduction or Collision :: Convergent Animation ::
Page 1 and 2: Plate Tectonics The Grand Unifying
Page 3 and 4: Elevations and Lithospheric Loading
Page 5 and 6: Why Are Continents Higher? • Cont
Page 7 and 8: Plate boundaries are zones of many
Page 9: The Major Plates of Earth’s Litho
Page 13 and 14: Divergent Boundaries • Sea-floor
Page 15 and 16: New Oceanic Crust at Mid-Ocean Ridg
Page 17 and 18: Why Are Mid-Ocean Ridges Elevated?
Page 19 and 20: Pillow Pillows In The Field Pillow
Page 21 and 22: Convergent Plate Boundaries: Subduc
Page 23 and 24: Convergent Boundaries • Accretion
Page 25 and 26: The Wadati-Benioff Zone • How do
Page 27 and 28: Subduction and Island Arcs Island A
Page 29 and 30: Transform Boundaries • Lithospher
Page 31 and 32: Transform Plate Boundaries - No Net
Page 33 and 34: SAF Aerial View
Page 35 and 36: Hot Spots • Not all volcanoes on
Page 37 and 38: The orientation of the Hawaiian arc
Page 40 and 41: The Birth of a Divergent boundary
Page 42 and 43: • The western U.S. - most of Neva
Page 44 and 45: What Drives Plate Motions? • The
Page 46 and 47: • Thanks to GPS and other geodeti
Page 48 and 49: Relative Plate Velocities Ignore re

Plate Tectonics: The Grand Unifying Theory of Geology

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?