My research focuses on the interplay between low-strain-rate crustal faults and the subduction zone plate interface鈥攕pecifically, what drives upper-plate deformation, and where, when, and how big past earthquakes were.
Many low-strain-rate faults are not well-characterized. They can be obscured by vegetation, development, or natural landscape modification. As a field geologist, I incorporate tools and methods from different disciplines within Earth sciences to answer these questions. In addition to mapping bedrock, surficial deposits, and landforms in the field, from lidar, and from Digital Surface Models (DSMs) collected via drone to identify recent surface ruptures, I excavate paleoseismic trenches to expose offset deposits in the subsurface and develop rupture histories using radiocarbon and luminescence dating.