Postglacial slip-rate increase on the Teton normal fault, northern Basin and Range Province, caused by melting of the Yellowstone ice cap and deglaciation of the Teton Range
Andrea Hampel et al., Ruhr-Universitaet Bochum, Institut fuer Geologie, Mineralogie und Geophysik, Universitaetsstr. 150, Bochum, Nordrhein-Westfalen 44801, Germany. Pages 1107-1110.
The Teton Range in the northeastern Basin-and-Range Province is famous for its high relief, with peaks up to 13,770 ft high (4,197 m), and a spectacular glacial geomorphology with deep U-shaped valleys. The rapid rise of this rugged mountain range in the last few million of years is related to repeated earthquakes on the Teton normal fault, which runs north-south along the mountain front. Today, the Teton fault represents a prominent seismic gap in the greater Yellowstone-Teton region; however, up to 50-m-high fault scarps and paleoseismologic data document that multiple earthquakes ruptured the Teton fault in the last 15,000 years, i.e. after the last glaciation. Hampel et al.s study shows that these earthquakes can be explained as a response to the melting of glaciers in the Teton Range and the large Yellowstone ice cap. More generally, their results im
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