3.1.5.2 Plate Tectonics Flashcards
structure
inner core, outer core, mantle, crust
asthenosphere
the semi molten larger area of the mantle
moho discontinuity
separates the crust from the mantle
plates colliding form…
subduction zones, earthquakes, volcanoes, fold mountains, deep sea trenches
plates torn apart form…
volcanoes, ocean trenches
alfred wegeners theory in 1912
single super-continent, pangaea, existed 300million years ago
later split into 2 continents- Laurasia in north, Gondwanaland in south
splitting of these formed todays continents
why plates move
continental drift
gravitational sliding/ridge push
slab pull
thermal plumes
gravitational sliding/ridge push
constructive boundaries
along ocean ridge, gravity pulls slopes
crust repeatedly torn causing shallow quakes
slab pull
destructive boundaries
gravitational pull of oceanic plate into mantle
subduction caused friction build so deep, shallow quakes
benioff zone
an inclined zone where many deep earthquakes occur, situated beneath a destructive boundary where oceanic crust being subducted