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The water that supplies the Santa Clara Valley Water District comes from various locations. Some of it comes from snowpack melt miles away. [3] This water is brought to the county through the many infrastructure projects in California, including the Federal Central Valley Project. [3] Santa Clara county also gets some of its water from recycled ...
Location: Santa Clara County, California: Coordinates: 1]: Type: Reservoir: Primary inflows: Cherry Canyon, [2] Pine Tree Canyon [3]: Primary outflows: Arroyo Calero [4]: Catchment area: 7.14 sq mi (18.5 km 2): Basin countries: United States: Managing agency: Santa Clara Valley Water District: Max. length: 2.2 miles (3.5 km): Surface area: 349 acres (141 ha): Water volume: 9,934 acre-feet ...
It is the second largest reservoir owned by the Santa Clara Valley Water District. [2] A 4,595-acre county park ("Coyote-Bear") surrounds the reservoir, [3] and provides camping (RVs and tents), fishing [4] ("catch-and-release"), picnicking, and hiking activities. Swimming is not allowed by order of the Santa Clara Valley Water District. [5]
The reservoir is managed by the Santa Clara Valley Water District (SCVWD) and has a current capacity of 3,465 acre-feet (4,274,000 m 3) of water. As currently managed by the SCVWD, flows are released during summer months which result in maintaining a wet channel for approximately 5.7 miles (9.2 km) downstream of the Reservoir (to Fremont Avenue ...
The Santa Clara Valley Water District accounts for 66% of the partners’ share. While the Bay Area agency is heavily invested, the largest water district in western Fresno County remains on the ...
In the early parts of the 20th century, the Santa Clara Valley was a vegetable and fruit growing region. Ground water was pumped heavily, leading to the Santa Clara valley being the first region recognized to be affected by land subsidence in the 1940s. [2] Between 1912 and 1966, artesian pressure levels dropped more than 200 feet (61 m).
In the 1920s, people discovered that Santa Clara Valley was sinking because of groundwater pumping. San Jose's elevation subsided 13 feet from 1910 to 1970s, correlated with a 250 feet decline in the underground water table. [7] [8] The valley's aquifers were also in danger of being ruined by saltwater infiltration. Local reservoirs were built ...
The reservoir was created in 1957 (68 years ago) () by the construction of the Uvas Dam [6] across Uvas Creek in the southern part of Uvas Valley. It is the fifth largest reservoir owned by the Santa Clara Valley Water District.