Oceanic Crust
Basaltic, usually near mid-ocean ridges and Subduction Zones.
- Higher density
- Thin
- Hotter
- Below ocean since its so dense High in:
- Magnesium
- Iron
Activities
- Oceanic to Oceanic Crust Convergence
- Oceanic to Continental Crust Convergence
- Oceanic to Continental Crust Transform
Onion Model
