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Los Angeles Aqueduct

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Los Angeles Aqueduct

Waterway extending for 375 km/233 mi across east-central and southern California. Built in 1908–13, its opening was a key event in the history of Los Angeles, as it allowed the San Fernando Valley to be cultivated and settled. The aqueduct taps the Owens River near Aberdeen, 42 km/26 mi north-northwest of Lone Pine, and then flows south along the east of the Sierra Nevada, then south-southwest across the western Mojave Desert, to the San Fernando Reservoir, north of Los Angeles.

Financial scandal and environmental controversy attended the inauguration of the Los Angeles Aqueduct; in planning its route, a series of questionable land deals were struck, and its construction dried out and depopulated the Owens Valley. Subsequently, when it was connected to streams feeding into Mono Lake in 1940–41, this lowered the level of the lake, sparking a long political wrangle over water use and despoilation of the environment.



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While his father drove mule teams, sometimes 16 hours a day, to haul materials and supplies for the Los Angeles Aqueduct, cement for the Old Ridge Route and hay for the multitude of mules owned by the city of Los Angeles, Frank's mother took care of business, the ranch and their son.
In November 1913, thousands watched as water flowed through the Los Angeles Aqueduct for the first time.
The Lower Owens River Project (LORP), a cooperative effort of the Los Angeles Department of Water and Power (LADWP) and the County of Inyo, will provide a steady flow of water to 62 miles of the Owens River below the Los Angeles Aqueduct Intake where the river has been essentially dry since the Aqueduct opened in 1913.
 
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