The global distribution of earthquakes and volcanoes follows distinct patterns along tectonic plate boundaries, with specific characteristics of oceanic and continental crusts playing crucial roles in seismic and volcanic activity.
Key points:
- Oceanic crust is thin (5-10km), dense, and composed of basaltic rock
- Continental crust is thicker (20-200km), less dense, and primarily made of granite
- Global distribution of earthquakes and volcanoes predominantly occurs along plate boundaries
- Hot spot volcanoes can form within plates, away from boundaries