Geological Society of America Special Paper 536, p. 53–66.Oviatt, C.G., Habiger, G., and Hay, J., 1994. The Bonneville flood — A veritable débâcle. Hundreds of skeletons of predators such as the saber-toothed cat and the dire wolf (The Huntington Mammoth lived about 10,500 years ago, very close to the time of the mammoth’s extinction. and Shroder, J.F., Jr., Eds., 2016. and Shroder, J.F., Jr., eds., Lake Bonneville: A scientific update.

The New Hudson Edition. The site is located at an elevation of 9,000 feet, making it the highest elevation find at the time (since this discovery, mammoth remains have been found in Colorado at 10,000 feet elevation).This mammoth was a very old individual, as indicated by tooth wear and arthritis in its bones. Isostatic rebound and palinspastic restoration of the Bonneville and Provo shorelines in the Bonneville basin, UT, NV, and ID.

659 p.Nelson, D.T.

Hydrology, Hydraulics, and Geomorphology of the Bonneville Flood. and Smith, G.R., 2016. Stratigraphy and chronology of Provo shoreline deposits and lake-level implications, late Pleistocene Lake Bonneville, eastern Great Basin, USA. Nature Geoscience 8, 175–176; Putnam, A.E., 2015. Elsevier. p. 292-351.Forester, R.M., 1987.

p. 105-126; Malde, H.E., 1968. Developments in Earth Surface Processes 20. Elsevier. Fish lived in Lake Bonneville; amphibians, waterfowl, and other birds inhabited its marshes; and animals such as buffalo, horses, bears, rodents, deer, camels, bighorn sheep, musk oxen, and mammoths roamed its shores. Utah Geological Society, p. 3-24.Oviatt, C.G. The Pony Express basaltic ash: A stratigraphic marker in late Pleistocene Lake Bonneville deposits, Utah. Age of the Cutler Dam Alloformation (Late Pleistocene), Bonneville basin, Utah. Developments in Earth Surface Processes 20.

Chapter 4. The Great Basin, with emphasis on glacial and post-glacial times – Climatic changes and pre-white man. in Gwynn, J.W., ed., Great Salt Lake: An overview of change. U.S. Geological Survey Monograph 1. Late Pleistocene mountain glaciation in the Lake Bonneville basin. Reinterpretation of the exposed record of the last two cycles of Lake Bonneville, western United States. p. 54-69.Oviatt, C.G. eds., North America and adjacent oceans during the last deglaciation. and Shroder, J.F., Jr., eds., Lake Bonneville: A scientific update. Special Publication of the Utah Department of Natural Resources, Utah Geological Survey. Collier & Son, New York. p. 221-291.Currey, D.R., 1982. It reached depths of 1,000 feet, compared to about 33 feet today and a 13-foot average depth). in Oviatt, C.G. [figure prepared by Oviatt, C.G., 2019; a similar map was published in reference 3].Gilbert, G.K., 1890. and Shroder, J.F., Jr., eds., Lake Bonneville: A scientific update. Great Salt Lake: A historical sketch. Late Quaternary changes in lakes, vegetation, and climate in the Bonneville basin reconstructed from sediment cores from Great Salt Lake.

They became extinct at the end of the Ice Age, about 10,000 years ago.Gravel quarries along the Wasatch Front contain the bones of many Ice Age animals. Palaeogeography, Palaeoclimatology, Palaeoecology 293, 41-50.Irving, W., 1868. and Shroder, J.F., Jr., eds., Lake Bonneville: A scientific update. and Nash, W.P., 1989. Elsevier. Geology of North America K-3, Geological Society of America, p. 261-276; Oviatt, C.G., 2017. Elsevier.

Danger Cave is a North American archaeological site located in the Bonneville Basin of western Utah around the Great Salt Lakes region, that features artifacts of the Desert Culture from c. 9000 BC until c. 500 AD. Lake Bonneville. 14,500 years ago, a breach in a sandstone wall, now known as Red Rock Pass, Idaho, resulted in the biggest flash flood this planet has ever known. and Wright, H. E., Jr. Developments in Earth Surface Processes 20. Horses and camels are both native to North America. Lake levels and climate reconstruction.

Boreas 42, 342–361.Atwood, G., Wambeam, T.J., and Anderson, N.J., 2016. Lake area constraints on past hydroclimate in the western United States: Application to Pleistocene Lake Bonneville. Quaternary Science Reviews 110, 166-171.Mifflin, M.D. and Shroder, J.F., Jr., eds., Lake Bonneville: A scientific update. One of the largest was Lake Bonneville; the modern-day Great Salt Lake is a remnant of that much larger body of water. Pluvial lakes and estimated pluvial climates of Nevada. in Stokes, W.L., ed., Guidebook to the Geology of Utah: The Great Salt Lake. and Wheat, M.M., 1979. and Jewell, P.W., 2015. New data on the isostatic deformation of Lake Bonneville: U.S. Geological Survey Professional Paper 454-E; Bills, B.G., Wambeam, T.J., and Currey, D.R., 2002. Quaternary Science Reviews 159, p. 169-189.Oviatt, C.G., 2015. Ostracodes in Pleistocene Lake Bonneville, eastern Great Basin, North America. Great Salt Lake: An overview of change. p. 462-503.Jewell, P.W., 2010. Mackay School of Mines, University of Nevada, Reno, NV. The fishes of Lake Bonneville: Implications for drainage history, biogeography, and lake levels.

Sediments of Great Salt Lake, Utah. Science Advances volume 4, issue 11, 10 p. https://advances.sciencemag.org/content/4/11; Putnam, A.E., 2015. Utah Geological Survey Miscellaneous Publication 14-3, 20 p.Crittenden Jr., M.D., 1963. The Gilbert episode in the Great Salt Lake basin, UT.

Nevada Bureau of Mines and Geology Bulletin 94. Elsevier. Journal of Paleolimnology 11, 19-30.Eardley, A.J., 1938. Geological Society of America Bulletin 101, 292-303.; Oviatt, C.G. The arrival of humans in the Lake Bonneville Basin has been set by archaeologists at about 10,000 years ago. Developments in Earth Surface Processes 20. in Oviatt, C.G. p. 7-32; Adams, K.D. Special Publication of the Utah Department of Natural Resources, Utah Geological Survey. in Oviatt, C.G. A glacial zephyr. Palaeogeography, Palaeoclimatology, Palaeoecology 76, 189-214.Oviatt, C.G., 2014. Nature Geoscience 8, 175–176.Antevs, E., 1948.