Scovern Hot Springs | |
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Agua Caliente Neills Hot Springs Hot Springs House | |
Location | Hot Springs Valley, Kern County, California |
Elevation | 2,490 ft |
Type | geothermal |
Discharge | 140-to-149 gallons per minute |
Temperature | 113°F /45°C |
Scovern Hot Springs | |
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Former settlement | |
Coordinates: 35°37′17″N118°28′27″W / 35.62139°N 118.47417°W | |
Country | United States |
State | California |
County | Kern County |
Elevation | 2,490 ft (759 m) |
Scovern Hot Springs (also known as Agua Caliente, Neills Hot Springs and Hot Springs House) is a thermal spring system, and former settlement in the Kern River Valley of the Southern Sierra Nevada, in Kern County, California. [1] [2]
The thermal springs in the area have been used historically by Native Americans and later by Spanish settlers for their balneotheraputic qualities. [3]
The Hot Springs Valley in Kern County was inhabited by the Palagewan people who lived along the Kern River's north fork. Other indigenous groups using the area were the Foothill Yokuts, Pahkanapil, Kawaiisu and Tübatulabal people. [4] [5]
A Tübatulabal village was located at the site of Scovern Hot Springs. [6] The Tübatulabal, a Uto-Aztecan-speaking people, are considered to have been the "first stewards of the region." Their complex societal structure and innovative trade network was based on seasonal patterns in relation to the land. [7] The Tübatulabal engaged in limited agriculture by harvesting local crops and herding animals in a semi-nomadic fashion. They maintained semi-permanent dwellings with rock foundations within their villages located throughout the valley. [4]
When the Spanish first arrived in the area in the late 1700s, they came in contact with the Tübatulabal and Kawaiisu in the region. During the early 1800s these indigenous people had limited trade-related transactions with the Euro-Americans. These cultural dynamics shifted when gold was discovered in 1848 at Sutter's Mill which brought thousands of miners to inland California including many to the Kern River and Lake Isabella valleys. [8] According to the Audubon California Kern River Preserve, the Tübatulabal first made contact with Francisco Garcés in 1776, and later with John C. Frémont in 1834, and with the Walker expedition in 1843. [4]
The Scovern Hot Springs are located in the South Fork Kern River region. For a time, the springs were known as Agua Caliente, and as Neills Hot Springs. [3]
The California Department of Conservation states that Scovern hot springs as well as several other hot springs along the Kern River have "historically been developed for resort/spa use." [9]
The former settlement of Scovern Hot Springs was located at the site of a geothermal spring system in the central area of Hot Springs Valley. In the 1800s it was a stop for horse-drawn stage coaches on the road between the town of Old Kernville and the railroad stop at Caliente. Ruins of the settlement that burned in 1971 could be seen until the mid-1990s when the remaining structure collapsed. [10]
In 1866, the hot springs became known to local settlers when the "Hot Springs House", a hotel and bathhouse, was built on the site to accommodate miners. [2] [11] Visalia W. Delta wrote in 1866 that the thermal waters were presented as curative of "peculiar inducements to invalids, especially those suffering from chronic diseases." She goes on to write that the owners at the time guaranteed the spring water was a "speedy cure of the most obdurate cases." During this time, the owners planned to develop the facilities for "families wishing to sojourn here" to offer them accommodations to stay for weeks at a time. The cost of room and board was $15 per week, including the use of the mineral baths. [3] In 1867 the "Ranch House" building was built at Scovern Hot Springs. [12] The hot mineral spring water at the bathhouse was purported to cure various ailments. For a time the facility was operated by a subsidiary of the Kern County Hospital. [2]
In 1902 John Neill purchased the "Hot Springs House", which at that time consisted of the hotel, a restaurant and a mineral spa. [11] In 1915 the resort was completed with the addition of a swimming pool. [3] Neill's wife Annie managed the hotel and its employees. John Neill's cousin, Robert Little, took care of the bath house. The old wooden mud-bath soaking tubs were updated with galvanized soaking tubs. Chinese cooks from the town of Kernville prepared food for guests. These upgrades brought tourists to the hot springs. [11] Eventually, boarders rented rooms month-to-month, dined in the restaurant and participated in events such as weekend square dances. [11]
The Neill family also bought the surrounding 840 acres which was farmed for alfalfa. The ranch raised sheep and cattle and a slaughterhouse was opened on-site. [13] [11] A local biographer wrote of the ranch and homestead that it had “ample barns and other out-buildings and [was] supplied with implements and appliances of every kind essential to diversified farming.” [14]
In 1929, Louis G. Scovern and his wife Edna [15] purchased the property, renamed it "The Scovern House". A swimming pool and additional bath houses were constructed at this time. [2]
In 1938, the hot springs resort spa was described as a popular watering place. [16] For a time a dude ranch was operated at Scovern Hot Springs. [17] In the late 1930s, Mr. and Mrs. H.A. Page managed the Scovern's Hot Springs Ranch. [12] In the 1930s and 40s the Sierra Roundup Rodeo took place at Scovern Hot Springs. [18] [19] The Scovern's daughter Pauline and her husband Johnny E. McNally, a ranch hand at the hot springs resort were married in 1936; McNally went on the produce the annual Sierra Rodeo Round-up held at Scovern Hot Springs. [20] In 1941 Scovern Hot Springs was called a "leading settlement Kern's 19th century mining days" by the Bakersfield Californian newspaper. [21]
In March, 1971 Scovern Hot Springs burned to the ground. [10] All of the resort buildings are gone, leaving only the natural hot spring. Visitors to the areas can observe the steam rising throughout the wetland fields across from the spring system. [2]
The hot water emerges from several spring sources in the Quaternary and Tertiary sedimentary rocks and alluvial material within the Kern Canyon geological fault zone. [3] [22]
The average temperature is 113 °F / 45 °C, flowing from the source at a rate of 140–to–149 gallons per minute. [23] Spring no. 1 emerges from the ground at 132 °F / 56 °C, at a rate of flow of 330 liters per minute (87 gallons per minute). [24] Two additional unnamed thermal wells are located near the primary Scovern hot springs. [25] Unnamed well no. 1 is 116 °F / 47 °C, and unnamed well no. 2 is 127 °F / 53 °C. [26] In addition to balneologic uses, the spring water was used for irrigation. [27]
Scovern Hot Springs is located in the South Fork Kern River region near Isabella [28] and 2.25 miles (3.6 km) north-northeast of Bodfish, [29] at an elevation of 2490 feet (759 m). [1] Scovern Hot Springs still appeared on maps as of 1943. [1]
The springs are located in the Kern Canyon fault zone [27] within the 225-acre Hot Springs Valley Wetlands complex. Due to the high-discharge rate of the springs, the water flows throughout the wetlands area at the daily average rate of 300,000 gallons. [30]
Kern County is a county located in the U.S. state of California. As of the 2020 census, the population was 909,235. Its county seat is Bakersfield.
Lake Isabella is a census-designated place (CDP) in the southern Sierra Nevada, in Kern County, California, United States. It is named after the Lake Isabella reservoir and located at its southwestern edge, 6 miles (9.7 km) south of Wofford Heights in the Kern River Valley.
The Kern River, previously Río de San Felipe, later La Porciúncula, is an Endangered, Wild and Scenic river in the U.S. state of California, approximately 165 miles (270 km) long. It drains an area of the southern Sierra Nevada mountains northeast of Bakersfield. Fed by snowmelt near Mount Whitney, the river passes through scenic canyons in the mountains and is a popular destination for whitewater rafting and kayaking. It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction.
Lake Isabella also called Isabella Lake, is a reservoir in Kern County, California, United States created by the earthen Isabella Dam. At 11,000 acres (4,500 ha), it is one of the larger reservoirs in California. Lake Isabella is located about 40 miles (64 km) northeast of Bakersfield, and is the main water supply for that city. It was formed in 1953 when the U.S. Army Corps of Engineers dammed the Kern River at the junction of its two forks. The area is in the southern end of the Sierra Nevada range and the lake itself is located in low mountains at an elevation of approximately 2,500 ft (760 m) where summer temperatures reach over 100 °F (38 °C) but low enough to avoid winter snows on the surrounding ridges. The former towns of Isabella and Kernville were flooded when the reservoir was created.
The Agua Caliente Band of Cahuilla Indians of the Agua Caliente Indian Reservation is a federally recognized tribe of the Cahuilla, located in Riverside County, California, United States. The Cahuilla inhabited the Coachella Valley desert and surrounding mountains between 5000 BCE and 500 CE. With the establishment of the reservations, the Cahuilla were officially divided into 10 sovereign nations, including the Agua Caliente Band.
State Route 178 is a state highway in the U.S. state of California that exists in two constructed segments. The gap in between segments is connected by various local roads and State Route 190 through Death Valley National Park. The western segment runs from State Route 99 in Bakersfield and over the Walker Pass in the Sierra Nevada to the turnoff for the Trona Pinnacles National Natural Landmark. The eastern segment runs from the southeasterly part of Death Valley to Nevada State Route 372 at the Nevada state line.
The Tübatulabal are an indigenous people of Kern River Valley in the Sierra Nevada range of California. They may have been the first people to make this area their permanent home. Today many of them are enrolled in the Tule River Indian Tribe. They are descendants of the people of the Uto-Aztecan language group, separating from Shoshone people about 3000 years ago.
Elizabeth Lake is a natural sag pond that lies directly on the San Andreas Fault in the northern Sierra Pelona Mountains, in northwestern Los Angeles County, southern California.
The Kern Canyon Fault is a dextral strike-slip fault (horizontal) that runs roughly around 150 km (93 mi) beside the Kern River Canyon through the mountainous area of the Southern Sierra Nevada Batholith. The fault was a reverse fault in the Early Cretaceous epoch during the primal stages of the Farallon Plate subduction beneath the North American Continental Plate and fully transitioned into a strike-slip shear zone during the Late Cretaceous.
The South Fork Kern River is a tributary of the Kern River in the Sierra Nevada of the U.S. state of California. It is one of the southernmost rivers on the western slope of the mountains, and drains a high, relatively dry plateau country of 982 square miles (2,540 km2) along the Sierra Crest. The upper South Fork flows through a series of rugged canyons, but it also drains a flat, marshy valley before joining the Kern River at Lake Isabella.
South Lake is an unincorporated community in the Kern River Valley, in Kern County, California. It is located 4.5 miles (7.2 km) west-southwest of Weldon, at an elevation of 2,887 feet (880 m).
Miracle Hot Springs is an unincorporated community in the Kern River Valley, in Kern County, California. It is located along the Kern River in the Sequoia National Forest 10 miles (16 km) west of Lake Isabella, California, at an elevation of 2,382 feet (726 m).
Canebrake Ecological Reserve is a 6,700-acre (27 km2) nature reserve in the South Fork Valley of Kern County, 20 miles (32 km) east of Lake Isabella, California. It is located in the Southern Sierra Nevada region.
The Kern River Valley is a valley and region of the Southern Sierra Nevada, in Kern County, California.
The Kern River Canyon is a canyon in Kern County, California. It is located in the Southern Sierra Nevada.
Sherman Pass is a mountain pass in California on the Kern Plateau in the Sequoia National Forest near the southern tip of the Sierra Nevada. It is traversed by Sherman Pass Road, which runs from Kern River Highway (M-99) at the North Fork of the Kern River on the west to Kennedy Meadow Road on the east.
Remington Hot Springs are an undeveloped thermal spring system located on the banks of the Kern River near Bodfish, California and Lake Isabella in the Sequoia National Forest in Kern County.
Delonegha Hot Springs are located in Kern County, California, United States, northeast of the city of Bakersfield and southeast of Glennville. Delonegha is one of several hot springs adjacent to the Kern River and State Route 178. The springs lie within the boundaries of Sequoia National Forest. Except for a brief period in the first years of the 20th century when there was a small resort at the site, the Delonegha springs have remained largely undeveloped.
Democrat Hot Springs, named for the Democratic political party, is a geothermally heated spring located 17 miles (27 km) northeast of Bakersfield, California, United States, on the south bank of the Kern River and on the north side of California State Route 178.
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