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Coulee is an unincorporated community in Mountrail County, North Dakota, United States, on the border of Ward County. [ 1 ] It is the location of Our Savior's Scandinavian Lutheran Church , which is listed on the U.S. National Register of Historic Places .
Mountrail County is a county in the northwestern part of North Dakota, United States.As of the 2020 census, the population was 9,809. [1] Its county seat is Stanley. [2] The county was originally created in 1873, then removed in 1892, annexed by Ward County.
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'.
Bismarck was founded by European-Americans in 1872 on the east bank of the Missouri River. It has been North Dakota's capital city since 1889, when the state was created from the Dakota Territory and admitted to the Union. [10] Bismarck is across the river from Mandan, named after a Native American tribe of the area. [11]
It is situated one mile north of State Route #50 and one quarter mile west of Ward County Highway #1 near Coulee, Mountrail County, North Dakota. The church and its cemetery were listed on the National Register of Historic Places in 2005. [1] [2] The single-story, wood-framed building has a vernacular front-gabled form with a vestibule tower in ...
Grand Coulee is two canyons, with an open basin in the middle. The Upper Coulee, filled by Banks Lake, is 25 miles (40 km) long with walls 800 to 900 feet (240 to 270 m) tall. It links to the Columbia River at Grand Coulee Dam and leads southward, through the surrounding highlands. The entry to the coulee is 650 feet (200 m) above the Columbia.
As of the census of 2010, there were 60 people, 27 households, and 14 families residing in the city. The population density was 333.3 inhabitants per square mile (128.7/km 2).
At Elm Coulee Field, the Bakken is only about 45 feet (15 m) thick and lies at depths of 8,500 to 10,500 feet (2,600–3,200 m), but horizontal wells penetrate 3,000 to 10,000 feet (900–3,000 m) of the reservoir rock, a porous dolomite of Devonian age that probably originated as a large carbonate bank on the western flank of the basin.