Quaternary history of the northeastern Bighorn Basin based on a climatically-controlled process-response model
Conference
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6577396
The highest surfaces and oldest Pleistocene sediments in the northeastern Bighorn Basin are associated with the 600 kya North Kane Ash. Subsequent climatically-induced periods of aggradation and incision produced the remaining geomorphic elements. Processes associated with a typical interglacial-glacial cycle include: (1) interglacial stability with Bighorn River alluviation, pedimentation, and eolian deposition; (2) late-interglacial to early-glacial incision; (3) alluvial fan extension and increased landslide development during glacial intervals; and (4) an early-interglacial return to more stable conditions. Frequent stream captures during interglacial times were caused by the out-of-phase relationships between the Bighorn River and its tributaries. Quaternary climates of a given type have not been of equal magnitude or duration in the northeastern Bighorn Basin. The most intense glacial climates from which sediments are preserved are believed to have occurred ca. 600 kya, 440 kya an d140 kya. An abnormally dry climate existed between 400 kya and 275 kya, while extremely wet interglacial conditions prevailed about 100 kya. The last complete climatic cycle was the Bull Lake. The subsequent Holocene interglacial has been unusually dry. Thus not all Pleistocene climates have been capable of generating terraces of extensive alluvial fans.
- Research Organization:
- Univ. of Southwestern Louisiana, Lafayette (USA)
- OSTI ID:
- 6577396
- Report Number(s):
- CONF-8510489-
- Conference Information:
- Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
- Country of Publication:
- United States
- Language:
- English
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Journal Article
·
Mon Feb 22 19:00:00 EST 2016
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·
OSTI ID:1260488
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Conference
·
Mon Aug 01 00:00:00 EDT 1983
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:6497341
High-precision provenance determination using detrital-zircon ages and petrography of Quaternary sands on the eastern Snake River Plain, Idaho
Journal Article
·
Wed Mar 31 23:00:00 EST 1999
· Geology
·
OSTI ID:343773
Related Subjects
58 GEOSCIENCES
580100* -- Geology & Hydrology-- (-1989)
ALLUVIAL DEPOSITS
CENOZOIC ERA
FEDERAL REGION VIII
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC HISTORY
GEOLOGIC MODELS
GEOLOGIC STRUCTURES
GEOLOGY
GEOMORPHOLOGY
GLACIERS
NORTH AMERICA
PALEOCLIMATOLOGY
PALEONTOLOGY
QUATERNARY PERIOD
SEDIMENTARY BASINS
SEDIMENTS
USA
WYOMING
580100* -- Geology & Hydrology-- (-1989)
ALLUVIAL DEPOSITS
CENOZOIC ERA
FEDERAL REGION VIII
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC HISTORY
GEOLOGIC MODELS
GEOLOGIC STRUCTURES
GEOLOGY
GEOMORPHOLOGY
GLACIERS
NORTH AMERICA
PALEOCLIMATOLOGY
PALEONTOLOGY
QUATERNARY PERIOD
SEDIMENTARY BASINS
SEDIMENTS
USA
WYOMING