Lake Tecopa
35°52′30″N 116°15′00″W / 35.87500°N 116.25000°W[1] Lake Tecopa is a
Hydrology
Lake Tecopa occupied the Tecopa Valley, a pear-shaped valley east of southern
At the time of the Bishop Tuff eruption, Lake Tecopa was about 100 metres (330 ft) deep.[10] The waters of the lake were salty and had a high pH,[11][10] inducing precipitation of calcite in the northern part of the lake where the Amargosa River flowed into it.[12] There is some indication that the centre of the lake was much more saline than its shores.[13] Salt lakes generally form when a lake has no outlet, so evaporation concentrates salts in the lake water until the lake contains saltwater.[14]
The
The catchment of the Amargosa River above Tecopa, California is presently about 8,000 square kilometres (3,100 sq mi). Later, after Lake Tecopa had disappeared, the river reached Death Valley and its Lake Manly,[10] dramatically increasing the supply of water to the latter.[19] Presently, the river is largely ephemeral except where it is fed by springs.[17]
Geography
The former lake basin is surrounded by various hills and mountain ranges, formed by rocks of
Presently, the towns of
Climate
Presently, the area of Lake Tecopa is a hot, dry desert with most precipitation occurring during summer. In Shoshone, California average temperatures are 19.5 °C (67.1 °F) and often exceed 45 °C (113 °F), with about 70 millimetres per year (2.8 in/year) of rainfall.[27][2] Under present-day climates, evaporation is too high and precipitation too low to allow the formation of lakes in the area.[9] 180,000 years before present, precipitation increased to 200–250 millimetres per year (7.9–9.8 in/year) and average temperatures decreased by 10.5 °C (50.9 °F), lifting the regional water tables.[27]
Sediments
Various sediments were emplaced in the lake, including
After the lake was breached, these deposits were deeply eroded and exposed,
Tufa deposits are found within the lake and partly embedded in its sediments; they were generated from carbonate precipitation within the lake, a process facilitated by the physical properties of the lake water.[31] Many of these tufa deposits occur where fault-controlled springs discharged water into the lake.[32]
Several tephra layers have been identified, including the 2.003 million years old Huckleberry Ridge Tuff, the 706,000 years old Bishop Tuff and the 602,000 years old Lava Creek Tuff[10][20] as well as the 2, 1.2-0.8 million years old Glass Mountain tuffs.[33] They form tuff layers which are very conspicuous in the lake sediments.[3]
Biology
A number of fossils were discovered in the sediments, including
History
Lake Tecopa existed during the
Extensive faulting of lake deposits makes it difficult to reconstruct its history.
At some point after 579,000 years ago, a 8 square kilometres (3.1 sq mi) large
About 200,000 - 150,000 years before present, the lake overflowed and disappeared.
The existence of the lake beds was described first by Levi F. Noble in 1926. In 1931, Eliot Blackwelder identified these lakebeds as the remnants of what he named Lake Tecopa.[17] The area of the former lake has been the subject of numerous studies comprising various fields of geology but also biology, and an important target for field studies and field trips.[53] Research in the paleoclimatic conditions of the region has received impetus from the Yucca Mountain nuclear waste repository, since the future climate of the region is important in establishing how secure the nuclear waste would be.[18][54]
References
- ^ a b Morrison 1999, p. 302.
- ^ a b Morrison 1999, p. 301.
- ^ a b c d Patterson 1987, p. 333.
- ^ a b Sheppard & Gude 1968, p. 1.
- ^ a b c d e Morrison 1999, p. 304.
- ^ a b Morrison 1999, p. 317.
- ^ Sheppard & Gude 1968, p. 4,5.
- ^ Larsen 2008, p. 619.
- ^ a b Gibert et al. 2011, p. 150.
- ^ a b c d e f g h i Nelson et al. 2001, p. 660.
- ^ Sheppard & Gude 1968, p. 33.
- ^ a b Sheppard & Gude 1968, p. 9.
- ^ Patterson 1987, p. 335.
- ^ Larsen 2008, p. 612.
- ^ a b Larsen 2008, p. 614.
- ^ a b Sheppard & Gude 1968, p. 4.
- ^ a b c d e f Morrison 1999, p. 303.
- ^ a b c d e Morrison & Mifflin 2000, p. 362.
- ^ Morrison 1999, p. 316,317.
- ^ a b c d e f g h Gibert et al. 2011, p. 149.
- ^ a b Nelson et al. 2001, p. 661.
- ^ a b Gibert et al. 2011, p. 148.
- ^ a b c Louie, John N.; Cetintas, Arif; Chekuri, Vijay; Corchuelo, William D.; Li, Li; Lei, Yutian; Mekala, Govardhan; Ozalaybey, Serdar; Raskulinecz, John. "Geophysical constraints on the cessation of extension and thickness of basin fill in Tecopa Valley, California". crack.seismo.unr.edu. The Nevada Seismological Laboratory. Retrieved 6 December 2017.
- ^ Morrison 1999, p. 330.
- ^ Reheis et al. 2019, p. 3.
- ^ Morrison & Mifflin 2000, p. 371.
- ^ a b Larsen 2008, p. 636.
- ^ Kodikara, McHenry & van der Meer 2023, p. 3.
- ^ Kodikara, McHenry & van der Meer 2023, p. 15.
- ^ Sheppard & Gude 1968, p. 2.
- ^ Nelson et al. 2001, p. 664,665.
- ^ Nelson et al. 2001, p. 669.
- ^ Reheis et al. 2019, p. 2.
- ^ Sheppard & Gude 1968, p. 6.
- .
- ^ Patterson 1987, p. 334.
- ^ Patterson 1987, p. 341.
- ^ a b Nelson et al. 2001, p. 659.
- ^ a b Morrison 1999, p. 311.
- ^ Reheis et al. 2019, p. 13.
- ^ Larsen 2008, p. 628.
- ^ Patterson 1987, p. 342.
- ^ Larsen 2008, p. 637.
- ^ Morrison & Mifflin 2000, p. 365,366.
- ISBN 9780813711997.
- ISSN 0091-7613.
- ^ Gibert et al. 2011, p. 157.
- ^ Morrison & Mifflin 2000, p. 368,369.
- ^ Reheis et al. 2019, p. 4.
- ^ Morrison 1999, p. 307.
- ^ Morrison 1999, p. 323.
- ^ Reheis et al. 2019, p. 26.
- ^ Reheis et al. 2019, p. 1.
- ^ Morrison 1999, p. 340.
Sources
- Gibert, L.; Alfaro, P.; García-Tortosa, F. J.; Scott, G. (1 April 2011). "Superposed deformed beds produced by single earthquakes (Tecopa Basin, California): Insights into paleoseismology". Sedimentary Geology. 235 (3): 148–159. .
- Kodikara, Gayantha R.L.; McHenry, Lindsay J.; van der Meer, Freek D. (February 2023). "Spectral mapping of zeolite bearing paleolake deposits at Lake Tecopa, California and its implications for mapping zeolites on Mars" (PDF). Geosystems and Geoenvironment. 2 (1): 100119. .
- Larsen, Daniel (1 June 2008). "Revisiting silicate authigenesis in the Pliocene–Pleistocene Lake Tecopa beds, southeastern California: Depositional and hydrological controls". Geosphere. 4 (3): 612. .
- Morrison, Roger Barron (January 1999). Lake Tecopa; Quaternary geology of Tecopa Valley, California, a multimillion-year record and its relevance to the proposed nuclear-waste repository at Yucca Mountain, Nevada | Cenozoic basins of the Death Valley region. Geological Society of America. .
- Morrison, Roger Barron; Mifflin, Martin D. (January 2000). "Lake Tecopa and its environs: 2.5 million years of exposed history relevant to climate, groundwater, and erosion issues at the proposed nuclear-waste repository at Yucca Mountain, Nevada". GSA Field Guide 2: Great Basin and Sierra Nevada. Vol. 2. Geological Society of America. pp. 355–382. ISBN 0-8137-0002-7.
- Nelson, Stephen T.; Karlsson, Haraldur R.; Paces, James B.; Tingley, David G.; Ward, Stephen; Peters, Mark T. (1 May 2001). "Paleohydrologic record of spring deposits in and around Pleistocene pluvial Lake Tecopa, southeastern California". GSA Bulletin. 113 (5): 659. ISSN 0016-7606.
- Patterson, R. T. (1 October 1987). "Arcellaceans and foraminifera from Pleistocene Lake Tecopa, California". The Journal of Foraminiferal Research. 17 (4): 333–343. ISSN 0096-1191.
- Reheis, Marith C.; Caskey, John; Bright, Jordon; Paces, James B.; Mahan, Shannon; Wan, Elmira (2019). "Pleistocene lakes and paleohydrologic environments of the Tecopa basin, California: Constraints on the drainage integration of the Amargosa River". GSA Bulletin. 132 (7–8): 1537–1565. S2CID 213373998.
- Sheppard, Richard A.; Gude, Arthur J. (1968). "Distribution and genesis of authigenic silicate minerals in tuffs of Pleistocene Lake Tecopa, Inyo County, California" (PDF). pubs.usgs.gov. doi:10.3133/pp597. Retrieved 6 December 2017.