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of 48
pro vyhledávání: '"Paul W. Jewell"'
Autor:
Paul W. Jewell
Publikováno v:
SN Applied Sciences, Vol 3, Iss 8, Pp 1-16 (2021)
Abstract Great Salt Lake of Utah is among the largest and most ecologically important water bodies in North America. Since the late 1950s, the lake has been divided into two hydrologically distinct water bodies by a rock-fill railroad causeway. Flux
Externí odkaz:
https://doaj.org/article/d77c1936f1c04d678e43e4043b05751a
Autor:
Jory Lerback, Erich U. Petersen, Christopher D. Bradbury, Jennifer V. DeGraffenried, Paul W. Jewell, Diego P. Fernandez
Publikováno v:
Quaternary Research. 99:114-127
To ascertain the provenance of water reaching wetlands in an area sustaining a population of Pleistocene–Holocene foragers, 87-strontium/86-strontium isotopic ratios (87Sr/86Sr) of mollusks from channels of the Old River Bed inland delta of central
Autor:
Cory Angeroth, Bonnie K. Baxter, William P. Johnson, Shu Yang, Gary E. Belovsky, Frank J. Black, Paul W. Jewell, Wayne A. Wurtsbaugh
Publikováno v:
Encyclopedia of Water
On this field trip we visit three sites in the Salt Lake Valley, Utah, USA, where we examine the geomorphology of the Bonneville shoreline, the history of glaciation in the Wasatch Range, and shorezone geomorphology of Great Salt Lake. Stop 1 is at S
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3727c274b6b324f98964c235c546146
https://doi.org/10.1130/2021.0060(03)
https://doi.org/10.1130/2021.0060(03)
Publikováno v:
Bulletin of the Seismological Society of America. 109:2198-2215
In an effort to better understand the Pleistocene history of the Wasatch fault zone, we evaluate the deformation and displacement of the Bonneville and Provo high‐stand shorelines of Lake Bonneville along the Wasatch Front. We apply an automated sh
Publikováno v:
Geomorphology. 318:390-403
Lake Bonneville was the largest of the late Pleistocene pluvial lakes that once filled part of the Great Basin of the interior western United States. As the lake reached its highest level at the Bonneville shoreline and overflowed, it eroded through
COSMOGENIC 10BE EXPOSURE DATING OF EROSIONAL LANDFORMS OF THE PROVO SHORELINE, LAKE BONNEVILLE BASIN
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Paul W. Jewell
Publikováno v:
Geomorphology. 253:135-145
Although the major shorelines of Pleistocene Lake Bonneville have been recognized for more than 100 years, less prominent shorelines have proven difficult to quantitatively identify and correlate since the time of G. K. Gilbert. By applying the Savit
Autor:
Daren T. Nelson, Paul W. Jewell
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 432:58-67
Distinct, mappable facies changes make the stratigraphic record of the shorezone of late Pleistocene Lake Bonneville the most robust indicator for past lake level oscillations. Unfortunately, clear stratigraphic evidence of transgressive and regressi
Publikováno v:
Geological Society of America Abstracts with Programs.