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Lewiston is home to California's third largest reservoir, the Trinity Dam; The Trinity River flows through the heart of Lewiston, directly under the Old Lewiston Bridge; Lewiston Lake is located along Trinity Dam Boulevard and is used primarily as a fishing and camping area, and not commonly used as a swimming destination owing to the frigid water.
Additional water comes from Lewiston Reservoir, supplied by the Trinity River, via the Clear Creek Tunnel, which comes from the bottom of Lewiston Lake. The California Office of Environmental Health Hazard Assessment has issued a safe eating advisory for any fish caught in the Whiskeytown Lake due to elevated levels of mercury. [1]
The Trinity River (Yurok: Hoopa or Hupa; Hupa: hun') is a major river in northwestern California in the United States and is the principal tributary of the Klamath River.The Trinity flows for 165 miles (266 km) through the Klamath Mountains and Coast Ranges, with a watershed area of nearly 3,000 square miles (7,800 km 2) in Trinity and Humboldt Counties.
The Trinity River as viewed from Reunion Tower in Dallas in August 2015. The Trinity River is a 710-mile (1,140 km) [2] river, the longest with a watershed entirely within the U.S. state of Texas. It rises in extreme northern Texas, a few miles south of the Red River. The headwaters are separated by the high bluffs on the southern side of the ...
The Stuart Fork Trinity River (also called Stewart's Fork) is a 14-mile (23 km) tributary of the Trinity River in the U.S. state of California. [1] The Stuart Fork Trinity river rises in the Trinity Alps from its headwaters at Emerald Lake and flows generally southeast into Trinity Lake , a reservoir formed by the Trinity Dam , just north of ...
The lake was completely filled with water from the Trinity River by 1963 and is the third largest lake in California with 145 miles (233 km) of shoreline. The area is the ancestral lands of several Native American tribes, most notably the Yurok and Hupa (Hoopa).
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The South Fork Trinity River begins as a small spring on the west slope of Chicago Rock near North Yolla Bolly Mountain, 4,460 feet (1,360 m) above sea level. [1] From there, it flows briefly west and turns to the north, receiving numerous small tributaries which drain a series of steep, forested valleys in the headwaters.