Paleoseismology

Paleoseismology is the study of ancient earthquakes by examining geological features and layers in the Earth’s crust. Researchers look for signs of past seismic activity, such as fault lines and displaced rocks, to understand how often and how strong earthquakes have occurred in a specific area. This information helps scientists assess the potential for future earthquakes, aiding in risk assessment and preparedness. Essentially, paleoseismology allows us to read the Earth’s history to better predict its future seismic behavior, enhancing our understanding of earthquake hazards.