Chapter 2: Plate Tectonics Flashcards
What is Plate Tectonics
Plate Tectonics states that the earth’s lithosphere is broken into a number of slabs of rock called plates
Who proved the theory of plate tectonics
Frederick Vine and Drummond Matthews in 1963
Who came up with earlier theories about plate tectonics
Continental Drift - Alfred Wegner 1912
Convection Currents - Arthur Holmes 1928
Mid-Ocean Ridges - Maurice Ewing 1947
Sea Floor Spreading - Harry Hess 1962
What is Continental Drift
Suggests that the continents are constantly moving across the planet by convection currents
What evidence is there to back up the theory of Pangaea (the supercontinent)
Continental Fit
Matching plant fossils
Matching rocks and mountains
Glacial deposits in countries with climates that would not create glaciers
What are convection currents
As the magma (6000 degrees C) becomes hotter it rises towards the crust. Upon reaching the upper mantle, it cools and becomes semi-molten. It then moves laterally before sinking again. As the magma moves sideways it rubs off the lithosphere causing friction which leads to plates separating, colliding and sliding past each other.
What is slab-pull force
When the edge of a plate begins to sink into the mantle, it then pulls the rest of the plate after it.