Abstract: What happens when 250 years of rapid ice loss induces one of the world's fastest crustal uplift rates directly above one of its fastest-slipping faults? Cryosphere-solid earth interactions in the Glacier Bay region, southeast Alaska (AGU Fall Meeting 2018)

What happens when 250 years of rapid ice loss induces one of the world's fastest crustal uplift rates directly above one of its fastest-slipping faults? Cryosphere-solid earth interactions in the Glacier Bay region, southeast Alaska

Chris Rollins^1,2, Jeffrey Todd Freymueller¹, Jeanne M Sauber³ and James L Davis⁴, (1)University of Alaska Fairbanks, Fairbanks, AK, United States, (2)University of Leeds, Leeds, United Kingdom, (3)NASA Goddard Space Flight Center, Geodesy and Geophysics Laboratory, Greenbelt, MD, United States, (4)Lamont-Doherty Earth Obervator, Lamont-Doherty Earth Observatory, Palisades, NY, United States

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