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
Outer core
2255 km thick
Liquid iron / nickel
Very dense
Temp: 3000-4500 C
Generates the magnetic field
Inner Core
Iron / nickel / mystery 3rd thing (oxygen or sulfur maybe)
Solid metal ball
1220 km radius
Temp: 5000 C
Seismic Waves
Caused by earthquakes/bombs
Travels through denser material faster
S-waves can’t travel through liquid
Creates shadow zones
Shadow zones
S-waves can’t travel through the outer core, so it leaves a ‘shadow’ opposite of the origin pt that is unaffected
Geodynamo
Self sustaining cycle caused by the magnetic fields that give no rise to more electric currents
Volcanos
Plates move in one direction over hot spots creating island chains. As the plate passes the hot spot the islands begin to erode
Rate of tectonic movements
1-20 cm a year
Magnetic field
Protects us from solar wind and radiation
Formed in the outer core
Auroras / Northern lights
Caused by electrically charged particles in solar wind hitting the electromagnetic field
Different colors caused by different gases hitting the atmosphere
Paleozoic Orogenic Belt
Appalachian mts
British Isles
Caledonia
When did the coast of Spain form
Jurassic period
Pyrenees Mountains
Formed during the Cretaceous period
Paleozoic era
Pangea
570-245 mya
Paleozoic orogenic belt
Mesozoic Era
Jurassic period
First Atlantic break
208-144 mya
Cretaceous period
Spain coast formed
Pyrenees mts formed
Southern Atlantic formed
144-66 mya