Deep Springs, California

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Deep Springs
Deep Springs Valley, California, view from Gilbert Pass (49291311177).jpg
Deep Springs Valley from Gilbert Pass
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Deep Springs
Location in California
Coordinates: 37°22′18″N117°59′06″W / 37.37167°N 117.98500°W / 37.37167; -117.98500
Country United States
Elevation
[1]
5,194 ft (1,583 m)

Deep Springs (formerly, Deep Spring) is a set of artesian springs in Inyo County, California that are used for irrigation, water supply, and livestock. The springs lie within the treaty territory of the Western Bands of the Shoshone Nation of Indians (Timbisha Band of Western Shoshone Indians). It is located in the northeastern section of Deep Springs Valley, 22 miles (35 km) east of Bishop, [2] 2.6 km (1.6 mi) north of Soldier Pass, and 6.4 km (4 mi) southwest of Chocolate Mountain (formerly Piper Mountain), [3] at an elevation of 5194 feet (1583 m). [1]

Contents

The area was originally home to the Deep Springs Valley Paiute prior to Euro-American settlement around the 20th century. Deeps Springs Valley has a semi-arid desert climate, and the springs create an environment with a variety of animal and plant life.

Deep Springs College is located in Deep Springs Valley, although not at the site of the springs. The students of Deep Springs College engage in a program emphasizing labor as a fundamental pillar of their studies. The students participate in a minimum of twenty hours of labor a week: milking cows, irrigating the farm, and learning about the land. The Deep Springs post office operated from 1881 to 1883 [2] and 1920 to 1953. [2] The springs, after which the town was named, are now called Buckhorn Springs. [2]

View of Deep Springs Lake Spring-fed pond along Deep Springs Fault zone, view south along base of the Lake Mountains east of Deep Springs Lake (19188285922).jpg
View of Deep Springs Lake

History & Natural Resources

The lake within the Deep Springs Valley, Deep Springs Lake, is also a rich source of evaporite minerals and mining material. However, the Deep Springs Lake is under-utilized because the nearby Owens Lake provides a more accessible source for mining. [4]

The Deep Springs are used for irrigation for agricultural operations and livestock in the area. There are several levees and ditches surrounding the lake that are presumed to improve the quality of life for grazing livestock and wildlife. The majority of the agriculture in the area is done by the students of Deep Springs College. The natural springs are also the main source of drinking water for the local area and Deep Springs College to meet daily water consumption needs. [5] The springs support all local animal and plant life.

Native People

John Wesley Powell talking with Paiute Chief John Wesley Powell Talks with the Paiute Chief, 1870s.jpg
John Wesley Powell talking with Paiute Chief

For thousands of years, the Deep Springs Valley Paiute, a distinct subgroup of the Northern Paiute people, inhabited Deep Springs, California. They established traditional cultural practices and separated themselves from other Paiute groups in nearby Owens and Fish Lake valleys. [6] Living in this remote and arid region, they adapted to the environment by developing an expansive knowledge of local plants, water sources, and hunting methods. They lived in the valley long before Euro-American settlers started to move into the area during the 20th century.

The Deep Springs Valley Paiute made use of a strategy called “annual round,” where the movements and activities of a group of people were dependent upon seasonal availability of available resources. [7] During the fall and winter they gather seeds, roots, and pine nuts, and hunt large game, including deer and mountain sheep. Survival involved their ability to adapt to the harsh environment and to efficiently exploit local resources. In particular, it was essential to their food supply that the pine nut harvest provided them with sustenance through their winter months. [7]

Wildlife

Notable Animal Life

Black Toad Anaxyrus exsul 001.jpg
Black Toad
Western Snowy Plover Snowy Plover edit.jpg
Western Snowy Plover

The Deep Springs Valley is specifically marked as an "Important Bird Area" by the Eastern Sierra Audubon Society however, the notable wildlife extends to amphibians, insects, and mammals as well. [8] Some notable species include, the Western Snowy Plover ( Charadrius alexandrinus nivosus ) and the Black Toad ( Anaxyrus exsul ). [9] The black toad is only found within the Eastern Sierra region, at an estimated population of around 7800-9700. The Deep Springs Valley wetlands are surrounded by desert, making it impossible for the black toad and other native species that rely on water to expand beyond that area. [10] As for the snowy plover and other migratory species, Deep Springs Valley provides a sanctuary of water and resources, as they begin flying south for the fall and winter months. The wetlands surrounding Deep Springs Lake as well as the marshier areas within the valley contribute to a more diverse ecosystem with an otherwise dry and arid climate.

Notable Plant Life

Deep Springs is also home to an assortment of plants. Around the main circle, there are Lemon Balm ( Melissa officinalis ) and Mullein ( Verbascum thapsus ). In rocky areas, there are Beavertail Cactus ( Opuntia basilaris ), Prince’s Plume ( Stanleya pinnata ), and Indigo Bush ( Psorothamnus arborescens var. minutifolius ). On the dry valley floor, there is Fourwing Saltbush ( Atriplex canescens ) and Hopsage ( Grayia spinosa ). On the wetter valley floor, there are Rabbitbrush ( Chrysothamnus greenei and viscidiflorus ), Antelope Bitterbrush ( Purshia tridentata var. glandulosa ), and Sagebrush ( Artemisia tridentata ssp. tridentata ).

Climate

Deep Springs Valley has a semi-arid desert climate with hot, dry summers and cold, dry winters—very similar to surrounding areas.

In the summer, temperatures at the Deep Springs reach maximums around 91.8 °F (33.2 °C) and minimums around 54.1 °F (12.3 °C). [11] In the winter, temperature maximums around 51.3 °F (10.7) and minimums around 7.7 °F (-7.7 °C). [11]

Year-round precipitation is sparse, with an annual total of 6.63 inches (16.84 cm). [11] Despite the low precipitation, occasional summer thunderstorms sometimes bring brief rainfall. [12]

Related Research Articles

<span class="mw-page-title-main">Inyo County, California</span> County in California, United States

Inyo County is a county in the eastern central part of the U.S. state of California, located between the Sierra Nevada and the state of Nevada. In the 2020 census, the population was 19,016. The county seat is Independence. Inyo County is on the east side of the Sierra Nevada and southeast of Yosemite National Park in Central California. It contains the Owens River Valley; it is flanked to the west by the Sierra Nevada and to the east by the White Mountains and the Inyo Mountains. With an area of 10,192 square miles (26,400 km2), Inyo is the second-largest county by area in California, after San Bernardino County. Almost half of that area is within Death Valley National Park. However, with a population density of 1.8 people per square mile, it also has the second-lowest population density in California, after Alpine County.

<span class="mw-page-title-main">Bishop, California</span> City in California, United States

Bishop is a city in California, United States. It is the most populous place and the only incorporated city in Inyo County. It is located near the northern end of the Owens Valley within the Mojave Desert, at an elevation of 4,150 feet (1,260 m). The city was named after Bishop Creek, flowing out of the Sierra Nevada range; the creek was named after Samuel Addison Bishop, a settler in the Owens Valley. Bishop is a commercial and residential center, while many vacation destinations and tourist attractions in the Sierra Nevada are located nearby.

<span class="mw-page-title-main">Owens Valley</span> Valley in California, United States

Owens Valley is an arid valley of the Owens River in eastern California in the United States. It is located to the east of the Sierra Nevada, west of the White Mountains and Inyo Mountains, and is split between the Great Basin Desert and the Mojave Desert. The mountain peaks on the West side reach above 14,000 feet (4,300 m) in elevation, while the floor of the Owens Valley is about 4,000 feet (1,200 m), making the valley the deepest in the United States. The Sierra Nevada casts the valley in a rain shadow, which makes Owens Valley "the Land of Little Rain". The bed of Owens Lake, now a predominantly dry endorheic alkali flat, sits on the southern end of the valley.

<span class="mw-page-title-main">Owens Lake</span> Dry lake in the Owens Valley, California

Owens Lake is a dry lake in the Owens Valley on the eastern side of the Sierra Nevada in Inyo County, California. It is about 5 miles (8.0 km) south of Lone Pine. Unlike most dry lakes in the Basin and Range Province that have been dry for thousands of years, Owens held significant water until 1943, when much of the Owens River was diverted into the Los Angeles Aqueduct, causing Owens Lake to desiccate by 1926. In 2006, 5% of the water flow was restored. As of 2013, it is the largest single source of dust pollution in the United States.

<span class="mw-page-title-main">Mono–Inyo Craters</span> Volcanic chain in eastern California, United States

The Mono–Inyo Craters are a volcanic chain of craters, domes and lava flows in Mono County, Eastern California. The chain stretches 25 miles (40 km) from the northwest shore of Mono Lake to the south of Mammoth Mountain. The Mono Lake Volcanic Field forms the northernmost part of the chain and consists of two volcanic islands in the lake and one cinder cone volcano on its northwest shore. Most of the Mono Craters, which make up the bulk of the northern part of the Mono–Inyo chain, are phreatic volcanoes that have since been either plugged or over-topped by rhyolite domes and lava flows. The Inyo volcanic chain form much of the southern part of the chain and consist of phreatic explosion pits, and rhyolitic lava flows and domes. The southernmost part of the chain consists of fumaroles and explosion pits on Mammoth Mountain and a set of cinder cones south of the mountain; the latter are called the Red Cones.

<span class="mw-page-title-main">White Mountains (California)</span> Mountain range in California, United States

The White Mountains of California and Nevada are a triangular fault-block mountain range facing the Sierra Nevada across the upper Owens Valley. They extend for approximately 60 mi (97 km) as a greatly elevated plateau about 20 mi (32 km) wide on the south, narrowing to a point at the north, with elevations generally increasing south to north. The range's broad southern end is near the community of Big Pine, where Westgard Pass and Deep Springs Valley separate it from the Inyo Mountains. The narrow northern end is at Montgomery Pass, where U.S. Route 6 crosses. The Fish Lake Valley lies east of the range; the southeast part of the mountains are separated from the Silver Peak Range by block faulting across the Furnace Creek Fault Zone, forming a feeder valley to Fish Lake Valley. The range lies within the eastern section of the Inyo National Forest.

<span class="mw-page-title-main">Great Basin Desert</span> Desert in the western United States

The Great Basin Desert is part of the Great Basin between the Sierra Nevada and the Wasatch Range. The desert is a geographical region that largely overlaps the Great Basin shrub steppe defined by the World Wildlife Fund, and the Central Basin and Range ecoregion defined by the U.S. Environmental Protection Agency and United States Geological Survey. It is a temperate desert with hot, dry summers and snowy winters. The desert spans large portions of Nevada and Utah, and extends into eastern California. The desert is one of the four biologically defined deserts in North America, in addition to the Mojave, Sonoran, and Chihuahuan Deserts.

<span class="mw-page-title-main">California water wars</span> Conflict over water rights in California between 1902 and 2006

The California Water Wars were a series of political conflicts between the city of Los Angeles and farmers and ranchers in the Owens Valley of Eastern California over water rights.

<span class="mw-page-title-main">Carson River</span> River in Nevada, United States

The Carson River is a northwestern Nevada river that empties into the Carson Sink, an endorheic basin. The main stem of the river is 131 miles (211 km) long although the addition of the East Fork makes the total length 205 miles (330 km), traversing five counties: Alpine County in California and Douglas, Storey, Lyon, and Churchill Counties in Nevada, as well as the Consolidated Municipality of Carson City, Nevada. The river is named for Kit Carson, who guided John C. Frémont's expedition westward up the Carson Valley and across Carson Pass in winter, 1844. The river made the National Priorities List (NPL) on October 30, 1990 as the Carson River Mercury Superfund site (CRMS) due to investigations that showed trace amounts of mercury in the wildlife and watershed sediments.

<span class="mw-page-title-main">Walker River</span> River in Nevada, United States

The Walker River is a river in west-central Nevada in the United States, approximately 62 miles (100 km) long. Fed principally by snowmelt from the Sierra Nevada of California, it drains an arid portion of the Great Basin southeast of Reno and flows into the endorheic basin of Walker Lake. The river is an important source of water for irrigation in its course through Nevada; water diversions have reduced its flow such that the level of Walker Lake has fallen 160 feet (49 m) between 1882 and 2010. The river was named for explorer Joseph Reddeford Walker, a mountain man and experienced scout who is known for establishing a segment of the California Trail.

<span class="mw-page-title-main">Walker Lake (Nevada)</span> Lake in Nevada, United States

Walker Lake is a natural lake in the Great Basin in western Nevada in the United States. It is 11 mi (17 km) long and 5 mi (8 km) wide, in northwestern Mineral County along the east side of the Wassuk Range, about 75 mi (120 km) southeast of Reno. The lake is fed from the north by the Walker River and has no natural outlet except absorption and evaporation. The community of Walker Lake is found along the southwest shore.

<span class="mw-page-title-main">Colorado Desert</span> Subdivision of the larger Sonoran Desert, California

Colorado Desert is a part of the larger Sonoran Desert located in California, United States, and Baja California, Mexico. It encompasses approximately 7 million acres, including the heavily irrigated Coachella, Imperial and Mexicali valleys. It is home to many unique flora and fauna.

<span class="mw-page-title-main">Owens River</span> River in eastern California

The Owens River is a river in eastern California in the United States, approximately 183 miles (295 km) long. It drains into and through the Owens Valley, an arid basin between the eastern slope of the Sierra Nevada and the western faces of the Inyo and White Mountains. The river terminates at the endorheic Owens Lake south of Lone Pine, at the bottom of a 2,600 sq mi (6,700 km2) watershed.

<span class="mw-page-title-main">California Central Valley grasslands</span> Temperate grasslands, savannas, and shrublands ecoregion in California, United States

The California Central Valley grasslands is a temperate grasslands, savannas, and shrublands ecoregion in California's Central Valley. It a diverse ecoregion containing areas of desert grassland, prairie, savanna, riparian forest, marsh, several types of seasonal vernal pools, and large lakes such as now-dry Tulare Lake, Buena Vista Lake, and Kern Lake.

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.

<span class="mw-page-title-main">Black toad</span> Species of amphibian

The black toad, also known as the Inyo toad or Deep Springs toad, is a true toad that lives only in scattered oases in the Deep Springs Valley of Inyo County, California. In fact, its original scientific name, Bufo exsul, means "exiled toad", which refers to its species' isolation in a tiny spot in the high desert wilderness of the Californian Great Basin.

<span class="mw-page-title-main">Mono people</span> Ethnic group

The Mono are a Native American people who traditionally live in the central Sierra Nevada, the Eastern Sierra, the Mono Basin, and adjacent areas of the Great Basin. They are often grouped under the historical label "Paiute" together with the Northern Paiute and Southern Paiute – but these three groups, although related within the Numic group of Uto-Aztecan languages, do not form a single, unique, unified group of Great Basin tribes.

Manzanar was a town in Inyo County, California, founded by water engineer and land developer George Chaffey. Most notably, Manzanar is known for its role in the internment of Japanese Americans during World War II.

The Timbisha are a Native American tribe federally recognized as the Death Valley Timbisha Shoshone Band of California. They are known as the Timbisha Shoshone Tribe and are located in south central California, near the Nevada border. As of the 2010 Census the population of the Village was 124. The older members still speak the ancestral language, also called Timbisha.

<span class="mw-page-title-main">Lake Tecopa</span> Lake in California, USA

Lake Tecopa is a former lake in Inyo County, southern California. It developed during the Miocene and the Pleistocene within a tectonic basin close to the border with Nevada. Fed by the Amargosa River and some neighbouring washes, it eventually culminated to a surface area of 235 square kilometres (91 sq mi) around 186,000 years ago and left sediments. Afterwards, the Amargosa River cut a gorge out of the lake and into Death Valley with its Lake Manly, draining the lake. The present-day towns of Shoshone, California and Tecopa, California lie within the basin of the former lake.

References

  1. 1 2 "Deep Springs". Geographic Names Information System . United States Geological Survey, United States Department of the Interior.
  2. 1 2 3 4 Durham, David L. (1998). California's Geographic Names: A Gazetteer of Historic and Modern Names of the State. Clovis, Calif.: Word Dancer Press. p. 1159. ISBN   1-884995-14-4.
  3. "Chocolate Mountain". Geographic Names Information System . United States Geological Survey, United States Department of the Interior.
  4. "Deep Springs Lake Ecological Reserve". wildlife.ca.gov. Retrieved October 23, 2024.
  5. "Deep Springs College – Prepare for a life of service". www.deepsprings.edu. Retrieved October 23, 2024.
  6. "Eastern California Museum | Inyo County California". www.inyocounty.us. Retrieved October 23, 2024.
  7. 1 2 "Natural History of the White-Inyo Range "d0e33239"". publishing.cdlib.org. Retrieved October 23, 2024.
  8. "Deep Springs Valley IBA | Eastern Sierra Audubon". esaudubon.org. Retrieved October 22, 2024.
  9. "Deep Springs Lake Ecological Reserve". wildlife.ca.gov. Retrieved October 22, 2024.
  10. "Amphibian Conservation - Black Toad". wildlife.ca.gov. Retrieved October 23, 2024.
  11. 1 2 3 "Deep Springs College, California: Climate and Daylight Charts and Data". www.climate-charts.com. Retrieved October 23, 2024.
  12. "DEEP SPRINGS COLLEGE, CALIFORNIA Period of Record Monthly Climate Summary". wrcc.dri.edu. Retrieved October 23, 2024.

Reference bibliography

  • Waring, Gerald Ashley (1915). Springs of California. U.S. Geological Survey Water Supply Paper. Vol. 338. U.S. Government Printing Office. doi:10.3133/wsp338.