[en] Paleoseismology techniques have been applied across the CEUS (Central and Eastern United States) to augment seismic data and to improve seismic hazard analyses. Considering paleoseismic data along with historic data may increase the number of events and their maximum magnitudes (Mmax), which may decrease the recurrence time of seismic events included in hazard calculations. More importantly, paleoseismic studies extend the length of the earthquake record often by 1000s–10,000s of years and reduce uncertainties related to sources, magnitude, and recurrence times of earthquakes. The CEUS Seismic Source Characterization (Technical Report, [108]) uses a lot of paleoseismic data in building the source model for seismic hazard analyses. Most of these data are derived through study of paleoliquefaction features. Appendix E of the Technical Report compiles data from ten distinct regions in eastern North America where paleoliquefaction features have been used to improve knowledge of regional seismic history. These regions are shown. Paleoliquefaction data can significantly impact seismic hazard calculations by better defining earthquake sources, Mmax for those sources, and recurrence rates of large earthquakes