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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 ...
Catchment area: 345 sq mi (894 km 2) Basin countries: United States: Managing agency: Santa Clara Valley Water District: Surface area: 288 acres (1.17 km 2) Water volume: 10,000 acre⋅ft (0.012 km 3) Surface elevation: 440 ft (134 m) References [1] [2]
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 imports 55% of its water. Much of that, including both federal and state contracts, is already stored at San Luis Reservoir and arrives at treatment ...
Thus, Lower Silver Creek used to begin southwest of where Lake Cunningham is today, but now its source is regarded as just north of this artificial lake by the Santa Clara Valley Water District (now Valley Water) at the confluence of Thompson Creek and Flint Creek. In the 1970s, Upper Silver Creek flows were shunted due west into a flood ...
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]
In 2006, an Aquatic Habitat Assessment and Limiting Factors Analysis commissioned by the Santa Clara Valley Water District concluded that the key factor limiting smolt production within the study area (San Francisquito Creek mainstem and Los Trancos Creek) and potentially throughout the watershed, is a lack of suitable winter refuge in deep ...
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 ...