Here's a breakdown:
* Convergent boundaries: Where plates collide. This is where most of the world's largest and most destructive earthquakes occur. Examples include the Pacific Ring of Fire, the Himalayas, and the Andes Mountains.
* Divergent boundaries: Where plates pull apart. These are generally associated with less powerful but more frequent earthquakes. Examples include the Mid-Atlantic Ridge and the East African Rift Valley.
* Transform boundaries: Where plates slide past each other. This can cause powerful earthquakes, as seen in the San Andreas Fault in California.
While the majority of earthquakes occur along plate boundaries, there are instances of intraplate earthquakes which happen within a plate, away from the boundaries. These are less common but can still be significant, like the 1811-1812 New Madrid earthquakes in the United States.
It's important to remember that the distribution of earthquakes isn't perfectly uniform even within plate boundaries. Specific areas with more fault lines or different types of plate interactions can have higher earthquake activity.
