Quaternary Bear River Paleohydrogeography Reconstructed from the 87Sr/86Sr Composition of Lacustrine Fossils
Diverted from its former course to the Pacific Ocean by basalt flows in Gem Valley, Idaho, the Bear River presently flows south into the Bonneville Basin. Constraining the timing of the river's diversion is pivotal to understanding the hydrologic budgets, and thus the climatological implication...
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| Format: | Others |
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DigitalCommons@USU
1997
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| Online Access: | https://digitalcommons.usu.edu/etd/4424 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=5451&context=etd |