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Learn about Alfred Wegener, the German scientist who first proposed the theory of continental drift and the existence of a super-continent. Explore the lithosphere, asthenosphere, and tectonic plates, and discover how they are responsible for geological activity at plate boundaries.
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Plate Tectonics Carrie Armstrong, Erin Rickert, Lydia Nguyen, Emmy Penquite
German Scientist • First to actively pursue the idea of a super-continent • Also came up with the theory of continental drift Alfred Wegener
How he got started: • The first clue Wegener had was the matching coast lines • he said they were almost like pieces of a jigsaw puzzle • Then noticed that other continents seemed to fit together to
Lithosphere • outer part of the Earth • Includes the crust and the mantle • about 100 km thick lithosphere
Asthenosphere • The ductile part of the earth just below the lithosphere • Includes the lower mantle • Referred to as hot plastic • About 180 km thick asthenosphere
Tectonic Plates • The tectonic plates glide over the asthenosphere at relates ranging from 1-16cm per year • Movement resembles ice drifting across a pond
Continental Drift • The continents and ocean basins make up the upper parts of the plates • As the plates glide the ocean and continents move with it • link
Geological activity • Most of this activity occurs at plate boundaries • Three types of plate boundaries exist • 1. divergent • 2. convergent • 3. transform