Paper No. 3
Presentation Time: 2:15 PM
TECTONIC AND SURFACE PROCESSES PRODUCE EARTH’S HIGHEST COASTAL MOUNTAINS
ENKELMANN, Eva, Department of Geology, University of Cincinnati, 500 Geology Physics Bldg., Cincinnati, OH 45221, KOONS, Peter O., Department of Earth Sciences, University of Maine, 5790 Bryand Global Sciences Center, Orono, ME 04469, PAVLIS, Terry L., Geological Sciences, University of Texas at El Paso, 500 W. University Ave, El Paso, TX 79968, BARKER, Adam, Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, HALLET, Bernard, Earth and Space Sciences and Quaternary Research Center, University of Washington, Seattle, WA 98195, ELLIOTT, Julie, Earth, Atmospheric, and Planetary Sciences, Purdue University, 550 Stadium Mall Drive, West Lafayette, IN 47907, FALKOWSKI, Sarah, Department of Geology, University of Tuebingen, Wilhelmstrasse 56, Tuebingen, 72074, Germany, GARVER, John I., Geology Department, Union College, 807 Union ST, Schenectady, NY 12308, PAVLIS, Gary L., Department of Geological Sciences, Indiana University, Bloomington, IN 47405 and RUPPERT, Natalia, Geophysical Institute, University of Alaska, Fairbanks, AK 99775, eva.enkelmann@uc.edu
Investigations of tectonic and surface processes have shown a clear spatial coincidence between the distribution of climate-influenced erosion and of long-term uplift and exhumation of rocks in many active mountain belts. Evaluation of the driver for exhumation and the understanding of key feedback mechanisms are complicated partly because climate has changed significantly in the late Cenozoic. The effects of climate change are particularly pronounced at high latitude where modern climate change is largest and where the growth and decay of enormous ice masses during the last ~2.5 Myr have profoundly affected the landscape.
A synthesis of new and published thermochronology data in the St. Elias Mountains reveals large spatial and temporal differences in rates and amounts of exhumation along the strike of the Yakutat – North American collision zone. The region of the indenting Yakutat plate corner, where dextral transform motion transitions to convergence, is the focal point for deformation, erosion, and exhumation. This region is currently characterized by the highest topography in the region and large ice fields that fuel fast moving glaciers (the Seward and Hubbard). The data reveal that the region was undergoing extremely rapid exhumation between ~4–2 Ma; it slowed down sometime after 2 Ma. Moreover, the most rapid exhumation shifted towards the south during the Pleistocene; currently it occurs at the southern flanks of the orogenic corner in the region between Icy Bay and Yakutat Bay. This is the region where geodynamic models predict very high strain rates and rapidly changing kinematics as thrust systems from the transpressional Fairweather transform converge into the central thrust belt producing rapid but shallow uplift and exhumation in a band that parallels the active thrust front. This thrust front coincides with largest GPS-constrained shortening rates, concentrated seismicity and the greatest erosive potential. The synthesis of geophysical, geological and surface process data, as well as model results, helps elucidate the evolving interplay of erosion and tectonics of the colliding Yakutat microplate, illuminating in particular, the important roles of crustal rheology, glaciers and climate.
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