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Coulee City was commonly known as McEntee’s Crossing of the Grand Coulee in the 19th century. In 1881, Philip McEntee, after helping a group of surveyors trying to lay down a road, built the first log cabin around Coulee City. Other important pioneers soon followed in the following years. [4] The town was named after nearby Grand Coulee. [5]
Aerial view from the south with Grand Coulee located centrally, Electric City to the left and Coulee Dam to the right. According to the United States Census Bureau, the city has a total area of 1.29 square miles (3.34 km 2), of which, 1.19 square miles (3.08 km 2) is land and 0.10 square miles (0.26 km 2) is water.
The Lower Grand Coulee is over a mile and a half wide in places with sheer basalt rock walls rising 900 feet over the coulee floor. State Highway 17, Coulee Corridor-National Scenic Byway, runs through Soap Lake and up the floor of the canyon heading towards Grand Coulee Dam and Canada. Of the five lakes existing along the Coulee Corridor, Soap ...
Coulee Dam was officially incorporated as a town on February 26, 1959. It is the headquarters of Lake Roosevelt National Recreation Area and home to one of the world's largest man-made piles of sand, a 12,000,000-cubic-yard (9,200,000 m 3 ), 230-foot (70 m)-high hill remaining from dam construction.
Grand Coulee is a large coulee on the Columbia River Plateau.This area has underlying granite bedrock, formed deep in the Earth's crust 40 to 60 million years ago. The land periodically uplifted and subsided over millions of years giving rise to some small mountains and, eventually, an inland sea.
A view through a coulee in Alberta, with steep but lower sides, and water in the bottom. Coulee, or coulée (/ ˈ k uː l eɪ / or / ˈ k uː l iː /), [1] is any of various different landforms, all of which are kinds of valleys or drainage zones. The word coulee comes from the Canadian French coulée, from French couler 'to flow'.
Banks Lake is a 27-mile-long (43 km) reservoir in central Washington in the United States.. Part of the Columbia Basin Project, Banks Lake occupies the northern portion of the Grand Coulee, a formerly dry coulee near the Columbia River, formed by the Missoula Floods during the Pleistocene epoch.
Moses Coulee is the second-largest and westernmost canyon of the Channeled Scablands, located about 30 kilometres (19 mi) to the west of the larger Grand Coulee. This water channel is now dry, but during glacial periods, large outburst floods with discharges greater than 600,000 m 3 /s (21,000,000 cu ft/s) carved the channel. [ 1 ]
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