Geological Field Trips in Southern Idaho, Eastern Oregon, and Northern Nevada
Geological Field Trips in Southern Idaho, Eastern Oregon, and Northern Nevada Edited by Kathleen M. Haller and Spencer H. Wood Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2004-1222 U.S. Department of the Interior U.S. Geological Survey 68 Geologic Field Trips to Central and Southwestern Idaho, Central Nevada, and Eastern Oregon Late Pleistocene Alpine Glaciation in the Southeastern Sawtooth Mountains, Idaho: Moraine Characteristics, Sediment Coring, and Paleoclimatic Inferences By Glenn D. Thackray1, Kari A. Lundeen2, and Jennifer A. Borgert3 Introduction maximum. We infer that the advances required reinvigora- tion of moisture transport into the northwestern interior of the United States. Glaciers descended the eastern flanks of the Sawtooth Mountains repeatedly during late Pleistocene time, con- structing an extensive moraine belt at the range front in the Sawtooth Valley. The glacial sequence and the numerous Setting and Context lakes it hosts preserve a detailed record of those fluctuations, themselves a reflection of complex climatic processes during The Sawtooth Mountains comprise one of the highest the last glaciation. In particular, we infer that the chronology ranges in central Idaho. The range trends roughly north-south derived to date reflects strong influences of Pacific moisture and rises to about 3,300 m, exposing Cretaceous granitic rocks delivery on the alpine glacial system. and Paleozoic metasedimentary wall rocks of the Idaho batho- The last glaciation involved dramatic reorganization of lith as well as Eocene granites of the Sawtooth batholith. Most oceanic, atmospheric, and cryospheric systems.
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