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- W2031204769 abstract "Multiple glaciation is evident in the north-central part of Yellowstone National Park; probably the youngest Pleistocene is Wisconsin in age. The valley formerly occupied by Lava Creek is pre-Wisconsin in age, and it has undergone little modification since that time. The valley contains old, deeply weathered granitic glacial boulders overlain by patches of fresh drift. During early Pleistocene time, Lava Creek occupied the valley between the Gardiner River and Blacktail Deer Creek and drained northward into the Yellowstone River. It has abandoned the pre-Wisconsin channel and drains into the Gardiner River at the west end of the old valley. This change was brought about by an ice lobe from the Lamar River region, probably in late Pleistocene time." @default.
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- W2031204769 date "1937-08-01" @default.
- W2031204769 modified "2023-09-25" @default.
- W2031204769 title "Evidence of Multiple Glaciation in the Northern Part of Yellowstone National Park" @default.
- W2031204769 doi "https://doi.org/10.1086/624586" @default.
- W2031204769 hasPublicationYear "1937" @default.
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