Deep Springs Valley

Deep Springs Valley is a high desert valley in the Inyo-White Mountains of Inyo County, California. It is east of the Owens Valley and the Sierra Nevada mountain range, and south of Fish Lake Valley, Nevada, near the California-Nevada state border.

California State Route 168 connects it to the Owens and Fish Lake valleys, crossing Westgard Pass to the west and Gilbert Pass to the north. To the northwest lies White Mountain Peak. To the east lies Eureka Valley, connected via Soldier Pass in the Piper Mountain Wilderness, which can be traversed on horseback but not by automobile.

Geography

Deep Springs Lake from the northwest.

Deep Springs Lake is a playa, a seasonal salt lake, generally drying in the summer to produce a salt pan, with surface water replenished in late spring with flows from nearby springs and snowmelt that travels the length of the valley from Wyman and Crooked creeks, which enter from the north. Birds, and birdwatchers, flock to the Lake during the spring and fall migrations. Surrounding the lake are numerous springs, some artesian, which gave the valley its name.

The springs are home to the Deep Springs Black Toad (Bufo exul, or "exile toad"), an endemic species that occurs only in Deep Springs Valley. In the 1980s, a second population of the toads was established several miles away at Antelope Springs as a defense against extinction due to unforeseeable disaster. The population of toads, however, appears to be stable, and even benefits from the presence of cattle that graze around the lake during the winter and spring.

Geology

On the hillsides of the southwestern end of the valley, lie the Poleta Folds, a distinctly visible example of crustal folding frequently studied by geology students from the University of California and California State University educational systems. The intensely folded and clearly visible layers comprise the Cambrian-aged Poleta formation. Several complex fault systems add to the challenge for geology students to unravel the area's history. The Poleta Folds field area is revered as one of the most complexly folded and faulted areas in California and has been used by generations of undergraduate-level geology students around the United States and Canada. During a typical summer one can often find near-established trails leading to the best outcrops.

Also easily visible at the base of the Inyo Mountains, in the southwestern end of the valley behind Deep Springs Lake, is a sizable faultline. Up to 40 feet in height, it is evidence of a massive earthquake estimated to have occurred about 2000 years ago.^[1] The fault is still active, but studies suggest that it slips about every 4000 years. Deep Springs Lake is intermittently filled and actively precipitating dolomite, understood to rarely occur in such conditions.

Population

It is the home of Deep Springs College, a nontraditional two-year liberal arts institution. There are also ruins of an early small mining establishment, White Mountain City, in the northwest corner of the valley.

See also

• Eureka Valley, Inyo County
• Eureka Valley Sand Dunes

• Swallenia
• Oenothera californica
• Category: Flora of the California desert regions

References

1. ^ Quaternary faulting history along the Deep Springs fault California, from Central Washington University. accessed 9-4-08