
Brandon Schmandt earned his B.A. from Warren Wilson College and his Ph.D. from the University of Oregon. He was a postdoctoral scholar at the California Institute of Technology (Caltech) and is now an assistant professor at the University of New Mexico.
Brandon’s research is characterized by artful integration of high-quality seismological imaging with geologic and tectonic information, and he has produced key insights into the structure and evolution of the North American continent. Brandon’s body wave tomography model for the western United States robustly synthesized data from the EarthScope Transportable Array and many other arrays. His collaborative work integrating this model with other seismic and geologic constraints has shed new light on varied processes, including the evolution of a segmented subducted Farallon slab, remnant microplates and slab windows, and lithospheric instabilities beneath the Colorado Plateau. Brandon has also produced evidence for a low-velocity layer on top of the western U.S. transition zone and the exciting observation of upwarping of the 660-kilometer discontinuity that correlates with a plume-like zone of low velocities in the mantle beneath the Yellowstone hot spot. This latter result is one of the best pieces of evidence to date for connection of a surface hot spot track with a lower mantle plume.
Brandon is continuing to innovate. Using a high-density exploration array in Long Beach, Calif., he recently resolved a sharp offset in Moho topography across the eastern edge of the California Inner Borderland, a result with significant tectonic implications. He is also pioneering in the field of fluvial seismology, studying the seismic signal of a dam release on the Colorado River as a tool for monitoring sediment transport.
To quote from his Aki Award nomination, “Brandon has already demonstrated technical innovations, keen intellectual curiosity, the drive and energy to produce at the highest levels, dedication to the new ethic of open access of data, and a gift for cross disciplinary collaboration, all with a sense of humility.”
—KAREN M. FISCHER, Department of Geological Sciences, Brown University, Providence, R.I.