Marie Barlett
Research Interests
My research is centered around the last major megathrust earthquake to occur along the Cascadia subduction zone in AD1700. Using fossil foraminiferal assemblages from three sites on Vancouver Island, British Columbia, I will estimate the coseismic subsidence associated with the AD1700 earthquake by comparing pre- and post-seismic paleo marsh elevations. High resolution subsidence estimates at the northern end of the Cascadia subduction zone are needed to refine earthquake dislocation models and gauge future hazard risk.
About Me
I am a second-year master’s student with a B.S. in Geology from the University of Georgia. I’m pursuing a M.S. in Marine Science and am interested in continuing to work in the fields of coastal geology and natural hazards after graduating from UNCW.