Barrett Dam is a concrete
arch-gravity dam
An arch-gravity dam or arched dam is a dam with the characteristics of both an arch dam and a gravity dam. It is a dam that curves upstream in a narrowing curve that directs most of the water pressure against the canyon rock walls, providing the ...
in southern
San Diego County
San Diego County (), officially the County of San Diego, is a county in the southwestern corner of the U.S. state of California. As of the 2020 census, the population was 3,298,634, making it California's second-most populous county and the f ...
,
California
California is a state in the Western United States, located along the Pacific Coast. With nearly 39.2million residents across a total area of approximately , it is the most populous U.S. state and the 3rd largest by area. It is also the ...
in the
United States
The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 U.S. state, states, a Washington, D.C., federal district, five ma ...
, forming Barrett Lake on
Cottonwood Creek. The dam is part of the city of
San Diego
San Diego ( , ; ) is a city on the Pacific Ocean coast of Southern California located immediately adjacent to the Mexico–United States border. With a 2020 population of 1,386,932, it is the eighth most populous city in the United States ...
's local water supply system.
Overview and operations
Barrett Dam is located in a narrow canyon just below the confluence of Cottonwood Creek and Pine Valley Creek, about east of downtown San Diego.
The dam is high above the riverbed and long, forming a reservoir with of usable capacity.
The dam contains of concrete.
The
spillway
A spillway is a structure used to provide the controlled release of water downstream from a dam or levee, typically into the riverbed of the dammed river itself. In the United Kingdom, they may be known as overflow channels. Spillways ensure t ...
is located on the face of the dam and is a stepped overflow structure controlled by gates. At maximum water levels the spillway capacity is approximately . To prevent
flash flood
A flash flood is a rapid flooding of low-lying areas: washes, rivers, dry lakes and depressions. It may be caused by heavy rain associated with a severe thunderstorm, hurricane, or tropical storm, or by meltwater from ice or snow flowing ...
s from overtopping the dam, the gates are left open during the rainy season from November 1 to April 1.
The dam's primary purpose is to store water for diversion through the Dulzura Conduit, a long concrete aqueduct which transfers water from the Cottonwood Creek basin to
Lower Otay Reservoir
Lower Otay Reservoir is a reservoir in San Diego County, Southern California. It is flanked by Otay Mountain to the southeast, the Jamul Mountains to the east, Otay Lakes Road and Upper Otay Reservoir to the north, and the city of Chula Vista to ...
. Water is released into the Dulzura Conduit via an outlet tower and a diameter pipe with a capacity of .
Water stored at Lower Otay passes through the Otay Water Treatment Plant before entering the municipal system. Barrett is one of two dams on Cottonwood Creek, the other being
Morena Dam upstream. Because Barrett is a deeper and narrower lake than Morena and experiences less evaporation, the city prioritizes water storage in Barrett. Water is moved downstream from Morena as long as storage space is available in Barrett. Resultantly, Barrett Lake is usually at a high level except during periods of extended drought.
History
Before there was a reservoir, the area was a valley that has been homesteaded by George Barrett in the 1870s. The first dam at the Barrett site was a high concrete diversion dam built in the 1890s as part of the Cottonwood-Otay System by the Southern California Mountain Water Company.
This dam's sole purpose was to feed the first Dulzura Conduit, a wooden flume that extended along the mountainside to the Lower Otay reservoir west. In 1913, the city of San Diego purchased this development for $2.5 million. Flooding in 1916 (ostensibly the work of the "rainmaker"
Charles Hatfield
Charles Mallory Hatfield (July 15, 1875January 12, 1958) was an American "rainmaker".
Early life
Hatfield was born in Fort Scott, Kansas on July 15, 1875. His family moved to Southern California in the 1880s. As an adult, he became a salesman f ...
) broke the dam at Lower Otay and overflowed the upstream Morena Dam, demonstrating the need for additional water storage capacity.
The city began construction on Barrett Dam in 1919,
["A History of the Dams and Water Supply of Western San Diego County," Lloyd Charles Fowler, University of California, 1953] under the direction of engineer Hiram N. Savage.
In December of that year, unusually heavy rainfall filled the reservoir behind the incomplete dam, very nearly causing its failure. Over the following few months, construction was hurried in order to keep up with the rising lake, which was only held back by wooden flashboards as the water level actually exceeded the height of the poured concrete for most of the construction period. Temporary sluiceways had to be maintained in order to drain excess water from the lake, which consistently threatened to overtop the dam. By the time the dam was completed in 1923 it was said that "the value of the water stored behind Barrett Dam by the time the structure was completed exceeded the entire cost of the dam".
Recreation
In order to protect water quality, recreational access to Barrett Lake is extremely limited. The lake is open only Wednesdays, Saturdays and Sundays, and visitors are required to take reservations. Fishing is allowed on a strict catch-and-release basis.
References
External links
Daily water levels tablefor Barrett and other San Diego County lakes
Dams in California
Dams completed in 1923
Arch-gravity dams
United States local public utility dams
1923 establishments in California
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