Earthquakes can occur in various locations around the world, but they are most commonly found along tectonic plate boundaries. These plate boundaries include:
1. Convergent Boundaries: Earthquakes occur where two plates collide or move towards each other. For example, the Pacific Ring of Fire, which is the region around the Pacific Ocean, experiences frequent earthquakes due to the presence of several tectonic plates interacting with each other.
2. Divergent Boundaries: Earthquakes occur where two plates move away from each other. These boundaries often form the seafloor ridges where new crust is created. The Mid-Atlantic Ridge and the East Pacific Rise are examples of divergent boundaries where earthquakes occur.
3. Transform Boundaries: Earthquakes occur where two plates slide past each other horizontally. The San Andreas Fault in California, United States, is a famous example of a transform boundary where frequent earthquakes occur.
It is important to note that earthquakes can occur in other regions as well, such as within continents or continental interiors, but they are less frequent in comparison to the areas near plate boundaries.
where do earthquakes normally occur
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