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The Mulholland Dam is a Los Angeles Department of Water and Power dam located in the Hollywood Hills of Los Angeles, California, east of the Hollywood Freeway.Designed with a storage capacity of 7,900 acre⋅ft (9,700,000 m 3) of water at a maximum depth of 183 feet (56 m), the dam forms the Hollywood Reservoir, which collects water from various aqueducts and impounds the creek of Weid Canyon.
The reservoir was created by the Mulholland Dam (built in 1924), designed by the Los Angeles Department of Water and Power—then named the Bureau of Water Works and Supply—as part of the city's water storage and supply system. [2] [3] The Hollywood Reservoir has appeared in films such as Earthquake (1974).
Sierra Madre Dam: Santa Anita Creek: Los Angeles: Los Angeles County Department of Public Works: 1928: Constant radius arch: 69: 21: 51: 63 Silver Lake Reservoir: Silver Lake Reservoir Dam: off-stream reservoir: Los Angeles: Los Angeles Department of Water and Power: 1907: Earth?? 2,400: 3,000 Silverwood Lake: Cedar Springs Dam: Mojave River ...
Mud was already flowing across the Hollywood Hills, damaging homes and forcing residents to flee. In Studio City late Sunday, a debris flow sent mud and other objects flowing down the 11900 block ...
The St. Francis Dam was built starting in 1924 (and through 1926), leading to the creation of a large reservoir in San Francisquito Canyon, and provided water for Los Angeles. The dam collapsed in 1928. Los Angeles flood in North Hollywood in 1938. The 1930s in particular saw rapid urban development in areas prone to river flooding. [19]
The Van Norman Dams, also known as the San Fernando Dams, were the terminus of the Los Angeles Aqueduct, supplying about 80 percent of Los Angeles' water, [5] until they were damaged in the 1971 San Fernando earthquake and were subsequently decommissioned due to the inherent instability of the site and their location directly above heavily populated areas.
A portion of the Port Hills. The Port Hills (Māori: Ngā Kohatu Whakarakaraka o Tamatea Pōkai Whenua) are a range of hills in Canterbury Region of New Zealand, so named because they lie between the city of Christchurch and its port at Lyttelton. They are an eroded remnant of the Lyttelton volcano, which erupted millions of years ago. [1]
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