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Convergent boundaries are best described when two tectonic plates are pushing into each other. They can have a subduction point where one of the plates goes under the other one. There is also a non-subduction boundary where both of the plates push up together to form mountain ranges.

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Divergent boundaries are when two tectonic plates are moving away from each other from convection currents. This causes rift valleys to form. These type of boundaries rarely cause earthquakes but do cause seafloor spreading.

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Strike-slip fault boundaries are boundaries that do not push up against each other or push apart, but instead move past each other. These Boundaries commonly cause earthquakes due to the rubbing of rock against rock. The most Famous strike-slip fault boundary is the San- Andreas fault line in California.