Plate Tectonics and the Ocean Floor Ch.2 Flashcards
Crust composition
low-density, mainly silicate minerals
mantle composition
mainly iron, and magnesium silicate minerals
core
high-density, mainly iron and nickel
Lithosphere
cool rigid shell, includes crust and upper mantle, about 100 km thick, forms tectonic plates
Asthenosphere
- relatively hot
- flows with high viscosity
- base of lithosphere to about 700km deep
Continenatl crust
granite (light coloured ingenous rock), density of 2.7 g/cubic cm, avg thickness of 35 km
oceanic crust
basalt (dark igneous rock), density of 3, avg thickness of 8km
Earthquake activity mirrors blank
tectonic plate boundaries
most large earthquakes occur where?
at subduction zones
Pangaea
one large continent existed 200 million years ago
Panthalassa
one large ocean (200 million years ago)
destructive margins (driving mechanism for plate motions)
at subduction zones at deep-sea trench
constructive margins
at mid-ocean ridges at spreading ocean ridge
litoshpere
rigid tectonic plates that float on ductile asthenosphere
paleomagnetism
study of earth’s ancient magnetic field