Gaviota Hot Springs | |
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Las Cruces Hot Springs Sulphur Springs | |
Location | Near Las Cruces, Santa Barbara County, California, U.S. |
Coordinates | 34°30′10″N120°13′06″W / 34.5027°N 120.2184°W |
Elevation | 500 feet (150 m) |
Type | geothermal |
Temperature | 99 °F (37 °C) |
Gaviota Hot Springs is a geothermal feature in Santa Barbara County, California, United States. The two pools are accessible from the Gaviota Peak trail in Gaviota State Park. [1] Gaviota Hot Springs is sometimes called Las Cruces Hot Springs or Sulphur Springs. [2] The hot springs lie within the Hot Springs Creek watershed, near the junction of U.S. Route 101 and California State Route 1. [3]
The springs were known to the indigenous peoples of the area, [4] and are located on land that was Rancho Las Cruces during the Mexican era of California. As early as 1880 there was a hotel at the village of Las Cruces advertising the medicinal benefits of the nearby hot sulfur springs. [5] The hotel was an adobe tavern on the side of the road that also served as the local brothel. [6]
A 1893 account of camping at the springs describes hanging hammocks from the sycamores around the pool, and needing to clear accumulated mud out of the roughly 8 feet (2.4 m) by 10 feet (3.0 m) bathing hole before it could be enjoyed by the group. [7] In 1896 the third edition of California of the South claimed that the Las Cruces Springs "had quite a local reputation for curing skin diseases and rheumatism." [8] In 1907 a promotional booklet published by California boosters described Las Cruces as one of three known hot springs in Santa Barbara County: [9]
Las Cruces Hot Springs [are] found in the Gaviota Cañon, a remarkable gorge that cleaves in twain the Santa Ynez Range, and down which a creek flows from the interior of the county. They are about 40 miles from Santa Barbara, some four miles the coast, and have been but slightly improved. It is a favorite camping-ground, and all the privileges of the springs are free to all who come.
The village of Las Cruces, located four miles north of Gaviota Pass, claimed circa 1913 that "The Hot Springs here are famous." [10] According to a 1917 report of the California state minerals bureau, the springs were located on the Las Cruces ranch and owned by the Hollister Estate Co. of Santa Barbara, and at that time "a group of 4 warm sulphuretted springs flowing about 50 gallons per minute issues from a clay bank on a hillside. The water is piped to the ranch houses for local use. Not utilized commercially." [11] One of the two pools is a man-made rock-and-concrete basin that was built by the Works Progress Administration during the New Deal era of the 1930s. [12] [4] During the same era, the Civilian Conservation Corps paved East Camino Cielo between the springs area and the San Marcos Pass. [13] The other pool has a natural bottom, and is fed by a separate spring vent, which is said to be the source of the lower pool's lukewarm temperature and the milky appearance of its water. [12] [14] Circa 1968, the springs were still associated with the Hollister Estate Company. [15] The springs were known as a litter-strewn party spot during the counterculture and underground days of the 1960s and 1970s. [4] [16]
The trail and springs are now regularly maintained by state park employees and volunteers; the springs and the park are open to the public during daylight hours. [17] [4] Mountain lions are among the wildlife that frequent the area. [18] [19] The springs are surrounded by native riparian-habitat plants including elderberry, willows, sycamores, and poison oak, [4] [14] and a naturalized palm tree that contributes an oasis vibe to the landscape. [17] A guide to hot springs in California and Nevada states, “Despite its murky appearance, this hot spring provides a great soak. The surrounding vegetation makes you feel like you’re in a jungle, and it keeps the location cool." [20]
The springs lie along the southern branch of the Santa Ynez Fault. [21] The water emerges from the source at about 99 °F (37 °C) [22] but cools before it reaches the pools. [2] The temperature also varies with the season. [2] The upper pool is typically both warmer and clearer than the lower pool, which it feeds. [23] The water contains sodium bicarbonate. [15] According to a U.S. government survey done around 1962, "spring issues in a dense thicket on hillside and is piped to concrete bathing tub." [15] The springs smell noticeably sulfurous, [14] and typically are described as being closer to warm than to hot. [4] [24]
U.S. government geologist Gerald A. Waring described Las Cruces Hot Springs in 1915: [25]
Las Cruces Hot Springs issue on a hillside about 18 miles (29 km) west of San Marcos Hot Springs and 4 miles (6.4 km) northward from Gaviota railroad station on the coast. Four warm springs here furnish about 50 US gallons (190 L; 42 imp gal) a minute of mildly sulphureted water and in two of the springs inflammable gas rises. A ledge of calcareous material back of the largest springs probably has been formed by deposition from the water. In 1908 there was a bathhouse at the largest spring, and the place was occasionally visited by campers. The topographic position of the springs is worthy of note, as they are in a little swale on the mountain side one half mile from and 400 feet above the main drainage canyon of this region. Thick-bedded sandstone here dips about 30° SW and strikes nearly in the direction of steepest slope.
One newspaper article from 1984 stated that Gaviota springs are "unusual inasmuch as tritium dating shows the water to be about 38 years old, coming from a depth of about 3,280 feet (1,000 m), with water temperature of 115 °F (46 °C) and a rate of flow of 25 US gallons (95 L; 21 imp gal) a minute." [17]
The Santa Ynez Mountains are a portion of the Transverse Ranges, part of the Pacific Coast Ranges of the west coast of North America. It is the westernmost range in the Transverse Ranges.
Gaviota State Park is a state park of California, United States. It is located in southern Santa Barbara County, California, about 33 miles (53 km) west of the city of Santa Barbara. One of three state parks along the Gaviota Coast, it extends from the Pacific coast to the crest of the Santa Ynez Mountains, and is adjacent to Los Padres National Forest. The 2,787-acre (1,128 ha) park was established in 1953.
The Santa Ynez River is one of the largest rivers on the Central Coast of California. It is 92 miles (148 km) long, flowing from east to west through the Santa Ynez Valley, reaching the Pacific Ocean at Surf, near Vandenberg Space Force Base and the city of Lompoc.
The Gaviota Tunnel is a tunnel on U.S. Route 101/State Route 1 (US 101/SR 1) completed in 1953 in the center of Gaviota State Park, 33 miles (53 km) northwest of Santa Barbara, California, on the Gaviota Coast. It is 420 feet (130 m) long and 17.5 feet (5.3 m) tall. Only the northbound lanes of US 101 pass through it, as the southbound lanes descend from Gaviota Pass through a narrow canyon to the west of the tunnel. Because it is the only major route between the Santa Barbara County South Coast and the Santa Ynez Valley, bicycles are allowed through it. There is a rest area for both southbound and northbound lanes on the southern end of the tunnel, the southernmost one along US 101.
San Marcos Pass is a mountain pass in the Santa Ynez Mountains in southern California.
Gaviota is an unincorporated community in Santa Barbara County, California on the Gaviota Coast about 30 miles (48 km) west of Santa Barbara and 15 miles (24 km) south of Buellton.
Los Encinos State Historic Park is a state park unit of California, preserving buildings of Rancho Los Encinos. The park is located near the corner of Balboa and Ventura Boulevards in Encino, California, in the San Fernando Valley. The rancho includes the original nine-room de la Ossa Adobe, the two-story limestone Garnier building, a blacksmith shop, a natural spring, and a pond. The 4.7-acre (1.9 ha) site was established as a California state park in 1949.
Gaviota Peak is a summit in the Santa Ynez Mountains in Santa Barbara County, California. It is located 10 miles (16 km) west of Santa Barbara, 16 miles (26 km) east of Point Conception and 2 miles (3.2 km) from the Pacific Ocean.
Rancho Las Cruces was a 8,888-acre (35.97 km2) Mexican land grant in the Santa Ynez Mountains of present-day Santa Barbara County, California given in 1837 by Governor Juan B. Alvarado to Miguel Cordero. The name means "the crosses". The grant was inland of present-day Gaviota Beach and the Gaviota Tunnel.
Las Cruces is a former settlement and an archaic placename in Santa Barbara County, California. It lies at the split between California State Route 1, which travels north to Lompoc, and U.S. Route 101, which travels north to Buellton. The two routes coincide on the highway to the south through the Gaviota Gorge to the Gaviota Coast. The community lies within area code 805.
The Sisquoc Formation is a sedimentary geologic unit widespread in Southern California, both on the coast and in mountains near the coast. Overlying the Monterey Formation, it is of upper Miocene and lower Pliocene age. The formation consists of claystone, mudstone, siltstone, shale, diatomite, and conglomerates, with considerable regional variation, and was deposited in a moderately deep marine environment at a depth of approximately 500–5,000 feet (150–1,520 m). Since some of its diatomites, along with those of the underlying Monterey Formation, are of unusual purity and extent, they can be mined as diatomaceous earth. France-based Imerys operates a mine in the Sisquoc and Monterey Formations in the hills south of Lompoc, California, the largest such operation in the world.
The Coldwater Sandstone is a sedimentary geologic unit of Eocene age found in Southern California, primarily in and south of the Santa Ynez Mountains of Santa Barbara County, and east into Ventura County. It consists primarily of massive arkosic sandstone with some siltstone and shale. Being exceptionally resistant to erosion, outcrops of the Coldwater form some of the most dramatic terrain on the south slope of the Santa Ynez Mountains, with immense white sculpted slabs forming peaks, hogback ridges, and sheer cliff faces.
The Matilija Sandstone is a sedimentary geologic unit of Eocene epoch in the Paleogene Period, found in Santa Barbara and Ventura Counties in Southern California.
The Juncal Formation is a prominent sedimentary geologic unit of Eocene age found in and north of the Santa Ynez Mountain range in southern and central Santa Barbara County and central Ventura County, California. An enormously thick series of sediments deposited over millions of years in environments ranging from nearshore to deep water, it makes up much of the crest of the Santa Ynez range north of Montecito, as well as portions of the San Rafael Mountains in the interior of the county. Its softer shales weather to saddles and swales, supporting a dense growth of brush, and its sandstones form prominent outcrops.
Wheeler Springs is an unincorporated community that grew around a set of sulphurated hot springs in Ventura County, California. It is located 6 miles north of the Ojai Valley, within Los Padres National Forest. It is named for Wheeler Blumberg, who founded the town in 1891, and the many natural hot springs.
Mission San Borja Hot Springs are located on the grounds of the historical Misión San Francisco Borja near the town of Rosarito in Baja California, Mexico.
The Gaviota Coast in Santa Barbara County, California is a rural coastline along the Santa Barbara Channel roughly bounded by Goleta Point on the south and the north boundary of the county on the north. This last undeveloped stretch of Southern California coastline consists of dramatic bluffs, isolated beaches and terraced grasslands.
Cañada Honda Creek is a perennial stream in Santa Barbara County, California, United States, that lies almost entirely within Vandenberg Space Force Base and meets the Pacific Ocean just north of Point Pedernales. Cañada Honda is part of the larger Santa Barbara coastal plain water resource subbasin.
Veronica Springs, also Veronica Medicinal Springs, was a cluster of natural springs along Arroyo Burro creek in Santa Barbara County, California, United States. Veronica spring water was not a therapeutic spa water or a table water but a medicinal mineral water with high magnesium levels. The waters had a yellowish tinge and a strongly purgative-laxative effect, and beginning around 1887, the water was bottled and sold as a health tonic. Veronica Water peaked as a brand in the 1910s. The springs were capped off in 1962.