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The Potholes Reservoir is part of the Columbia Basin Irrigation Project. It is formed by the O'Sullivan Dam and located in central Washington, in the United States. The reservoir is fed by water from Moses Lake, part of the Crab Creek basin. The area features several lakes (typically 30-70 yards wide and 10–30 feet deep).
Potholes State Park is a public recreation area on the southern shore of Potholes Reservoir, located 13 miles (21 km) south of Moses Lake and 13 miles (21 km) northwest of Othello in Grant County, Washington. The state park was created following the completion of the O'Sullivan Dam in 1949. The park's 773 acres (313 ha) include 6,000 feet ...
The northern half of the refuge, south of Potholes Reservoir, is a rugged jumble of cliffs, canyons, lakes, and remnants of lava flows. This part of the Scablands, known as the Drumheller Channels, is the most spectacularly eroded area of its size in the world and was designated as a National Natural Landmark in 1986. [4]
Moses Lake is a lake and reservoir along the course of Crab Creek, in the U.S. state of Washington. Moses Lake is part of the Columbia River basin, as Crab Creek is a tributary of the Columbia River. Although originally a shallow natural lake, Moses Lake was dammed in the early 20th century for irrigation purposes.
O'Sullivan Dam located near the bottom of Potholes Reservoir. O'Sullivan Dam (National ID # WA00268), one of the largest earthfill dams in the United States (200 ft/61 m high; 19,000 ft/5,791 m long; completed 1949), is on Crab Creek in the U.S. state of Washington, about 45 km south of Ephrata and 25 km south of Moses Lake.
Crab Creek is a stream in the U.S. state of Washington.Named for the presence of crayfish, [7] it is one of the few perennial streams in the Columbia Basin of central Washington, flowing from the northeastern Columbia River Plateau, roughly 5 km (3.1 mi) east of Reardan, west-southwest to empty into the Columbia River near the small town of Beverly.
Bretz recorded 150 distinct channels and over 180 rock basins in this region. Many of the low areas, including Upper Goose Lake, are filled by water seeping in through cracks in the basalt bedrock, which are connected with Potholes Reservoir to the north. [7]
Archbald Pothole is 38 feet (11.6 m) deep and 42 feet (12.8 m) wide at its maximum diameter.The pothole cuts through layers of sandstone, shale and coal.A pothole, in geologic terms, is a hole that is worn into the bedrock of a stream in strong rapids or at the base of a waterfall.
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