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Construction of Canyon Dam began in 1958 to provide both flood control and water conservation. Impoundment of the lake began in 1964, and the lake was filled to its conservation level in 1968. The dam was built by the Tencon Corporation of Fort Worth, Texas. The United States Army Corps of Engineers controls the physical operations; and water ...
Canyon Lake is a reservoir on the Guadalupe River in the Texas Hill Country in the United States. Canyon Lake is a U.S. Army Corps of Engineers reservoir formed on the Guadalupe River in Comal County by Canyon Dam, which is located about sixteen miles northwest of New Braunfels. The dam, lake, and all adjacent property are managed by the U.S ...
It was formed by the Mormon Flat Dam, which was completed in 1925 after two years of construction. Canyon Lake, with a surface area of 950 acres (380 ha), is the third and smallest of the four lakes created along the river. Two others, Apache Lake and Roosevelt Lake, are upstream. The fourth, Saguaro Lake, is downstream.
The reservoir is supplied by storm water runoff from the San Jacinto River and Salt Creek. Water from the reservoir feeds the Canyon Lake Water Treatment Plant, which provides approximately 10% of the domestic water supply in the Lake Elsinore and city of Canyon Lake area. Canyon Lake has an average depth of 20 feet (6.1 m).
Canyon Lake Gorge is a limestone gorge in Texas, which is around 1 mile (1.6 km) long, hundreds of yards (metres) wide, and up to 50 feet (15 m) or more deep, which was exposed in 2002 when extensive flooding of the Guadalupe River led to a huge amount of water going over the spillway from Canyon Lake reservoir and removing the sediment from ...
Newly discovered damage in Glen Canyon Dam would require releasing less water at low reservoir levels — a problem that increases water risks in the Southwest.
The run-off carried rubble to the Canyon Lake Dam creating a barrier in front of its spillway. [4] This resulted in the "increase in depth of water behind the dam of 11 to 12 feet," which caused the release of more water adding to the already moving floodwaters. [9]
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