In 1700, a massive earthquake struck the west coast of North America. Though it was powerful enough to cause a tsunami as far as Japan, a lack of local documentation has made studying this historic event challenging.
Benjamin Horton, Professor in the Institute of Marine and Coastal Science at Rutgers University, and colleagues have helped unlock this geological mystery using a fossil-based technique.
Their work provides a finer-grained portrait of this earthquake and the changes in coastal land level it produced, enabling modelers to better prepare for future events.