The study of plate boundaries and the frequency of past earthquakes in order to forecast earthquakes is known as

The study of plate boundaries and the frequency of past earthquakes in order to forecast earthquakes is known as

paleoseismology.

dilatancy.

moment magnitude.

paleontology.

geodesy.

A: Paleoseismology

Explanation:

Paleoseismology is the study of plate boundaries and the frequency of past earthquakes in order to discover their location, size, and timing. The focus of the paleoseismologist are deformation of landforms and sediments during earthquakes, which is useful to understand the regional patterns of tectonic deformation. This study is part of a broader field of earthquake geology.