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In the 2021 Census of Population conducted by Statistics Canada, Grand Coulee had a population of 606 living in 202 of its 209 total private dwellings, a change of -6.6% from its 2016 population of 649.
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.
This article is a list of historic places in rural municipalities of the province of Saskatchewan entered on the Canadian Register of Historic Places, whether they are federal, provincial, or municipal.
In the 2016 Census of Population, the RM of Coulee No. 136 recorded a population of 563 living in 183 of its 205 total private dwellings, a -3.3% change from its 2011 population of 582. With a land area of 843.69 km 2 (325.75 sq mi), it had a population density of 0.7/km 2 (1.7/sq mi) in 2016.
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'.
The Rural Municipality of Sherwood No. 159 (2016 population: 974) is a rural municipality (RM) in the Canadian province of Saskatchewan within Census Division No. 6 and SARM Division No. 2. In the south-central portion of the province, it surrounds the city of Regina , the provincial capital, and forms part of the Regina census metropolitan area .
Pense is a town of 603 residents (2021 census [4]) in the southern part of Saskatchewan, Canada. Heading west from Regina on the Trans Canada Highway, Pense is the first community with services. Other communities in the area include Grand Coulee, Belle Plaine, Disley, and Rouleau. Pense is approximately 30 kilometres (19 mi) from the city of ...
Hearts Hill, the most prominent feature in the Luseland district, is the most eastern outlier of the moraine fields, separating the Buffalo Coulee system that drains into the South Saskatchewan River valley, from the Grass Lake system that drains eastward into Tramping Lake. Finer glacial sediments along these valleys gave rise to the rich ...
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