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Continental drift
Alfred Wegener; he had evidence but no mechanism for how continents moved.
Evidence used by Wegener for continental drift
Fit of continents, matching fossils, similar rocks/mountains, glacial evidence.
Evidence supporting plate tectonics
Magnetic stripes on the seafloor.
Lithosphere
Rigid plates (crust + uppermost mantle) that move on the asthenosphere.
Asthenosphere
A weak, plastic layer in the upper mantle that the plates move on.
Oceanic crust
Thin, dense, basalt.
Continental crust
Thick, less dense, granite.
Divergent boundary
Forms mid-ocean ridges.
Convergent boundary
Forms subduction zones with trenches and volcanoes (oceanic-continental or oceanic-oceanic).
Transform boundary
The San Andreas Fault (plates slide past).