Earth’s interior & Plate Tectonics Flashcards
Alfred Wegner Discoveries
1924
Coastlines match
Rock type match
Appalachian mts
Glacial striations
Matching fossils
Alfred Wegner failure
Non-scientific/scholarly
German language barrier
German social barrier
Evidence on ocean floor
Henry Hess Discovery
1940s
Pacific Ocean floor has linear volcano chains (erosion/aging)
Deep trenches parallel to mts. & volcanos
1960s
Mid ocean ridge discovered
Marie Tharp & Bruce Heezen
Created physiographic map of ocean floor
Vine & DH Matthew
Plates diverge from separating center
Earth’s magnetic field reverses
Tectonic boundary 1
Divergent
<—>
Tectonic Boundary 2
Convergent OC><OC
OC will bend under OC
Tectonic Boundary 3
Convergent OC><CC
OC will bend under CC
Tectonic Boundary 4
Convergent CC><CC
CC crust will crumple against CC
Creates mts
Tectonic Boundary 5
Transform = parallel to another plate
Just sliding by
Continental Crust
35-45 km thick
Silicate rock material
Rock types: igneous, sedimentary, and metamorphic
Low density
Oceanic Crust
5-10 km thick
Young 0-320 million
Basaltic igneous rock & marine sediment
Denser than continental crust
Mantle
2900 km thick
Largest part of earth by volume
Solid, untra-mafic dense rock called peridotite
Main mineral - Bridgmanite
Upper/lower mantle split at 660 km deep
Behaves like plastic
Temp: 1000-3700 C
Geothermal Gradient
Temperature increases with depth