1. Tectonic plates on the surface of the earth’s crust are rafted around by **convection currents** (creating the 3 different types of plate boundaries) powered by **radioactive decay** in the boundary between the mantle and the core
2. As plates diverge, converge, or slide past each other, **pressure** builds up **between faults** that are locked together by irregularities and friction
3. Eventually the **pressure exceeds frictional resistance** and a **fault fails**, triggering in earthquake, and aftershocks **if other faults are stressed**
Convergent boundaries:
* Crust is **compressed**, creating **thrust** or **reverse** faults
* Hypocenter depth **varies**, **infrequent** earthquakes but **high magnitude** and **destructive**
Divergent boundaries:
* Crust is under **tension**, creating **normal faults**
* **Shallow** hypocenter, frequent earthquakes but low magnitude and **not** very destructive
Conservative boundaries:
* **Transform** faults
* **Shallow** hypocenter, failure usually happens along a **large section** of the fault so very destructive