Late Pleistocene glacial chronologies and paleoclimate in the northern Rocky Mountains
The geologic record of mountain glaciations is a robust indicator of terrestrial paleoclimate change. During the last glaciation, mountain ranges across the western U.S. hosted glaciers while the Cordilleran and Laurentide ice sheets flowed to the west and east of the continental divide, respectivel...
Main Authors: | , , , , , , |
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Format: | Text |
Language: | English |
Published: |
2021
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Subjects: | |
Online Access: | https://doi.org/10.5194/cp-2021-106 https://cp.copernicus.org/preprints/cp-2021-106/ |