An extinct lake with surviving remnants in western Nevada and northeast California. It was formed by heavy precipitation caused by Pleistocene glaciers but largely disappeared after the end of the epoch.
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La·hon·tan (lə-hŏn'tən)
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Ancient Lake Lahontan was a large endorheic lake that existed during the ice age, covering much of northwestern Nevada, extending into northeastern California and southern Oregon.
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At its peak approximately 12,700 years ago (during a period known as the "Sehoo Highstand"), the lake had a surface area of over 8500 square miles (22015 square kilometres), [1] with its largest component centered at the location of the present Carson Sink. The depth of the lake was approximately 900 feet[2] (290 m) at present day Pyramid Lake, and 500 feet (150 m) at the Black Rock Desert. Lake Lahontan, during this most recent glacial period, would have been one of the largest lakes in North America.[3]
Climate change around the end of the Pleistocene epoch led to a gradual desiccation of ancient Lake Lahontan. The lake had largely disappeared in its extended form by approximately 9,000 years ago. As the surface elevation dropped, the lake broke up into series of smaller lakes, most of which rapidly dried up leaving only a playa. These playas include the Black Rock Desert, the Carson Sink and the Humboldt Sink. The only modern day remnants existing as true lakes are Pyramid Lake and Walker Lake. Winnemucca Lake has been dry since the 1930s and Honey Lake periodically desiccates. The ancient shoreline is evidenced by tufa formations throughout the area.
Surprisingly, the watershed feeding Lake Lahontan is not thought to have been significantly wetter during its highstand than it is currently. Rather, its desiccation is thought to be mostly due to increase in the evaporation rate as the climate warmed.[citation needed] Recent computer simulations (using the DSSAM Model[4] and other techniques) indicate that if precipitation and evaporation rates within the watershed were maintained at their historical yearly maximum and minimum, respectively and if diversions of the Truckee River ceased, the Ice Age extent of Lake Lahontan could return.
The existence of the lake coincided roughly with the first appearance of humans in that region of North America. Archaeological evidence exists along the ancient lake shore of early human habitation.
The Lahontan cutthroat trout evolved as a predator species within the waters of Lake Lahontan, feeding on native chub and sucker. This subspecies of cutthroat trout survives today in tributary rivers of the Great Basin, and has been re-introduced to Pyramid Lake and Walker Lake after being extirpated during the 20th century.
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| Walker Lake (lake, Nevada) | |
| Carson Sink (geographical area, Nevada) | |
| Pyramid Lake (lake, Nevada) |
| What water temp do lahontan cutthroat live in? | |
| What do you do at the lake? | |
| What is an lake? |
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