1974
DOI: 10.4095/119895
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Guide to the geology of Elk Island National Park: the origin of its hills and other scenery

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1978
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“…Elk Island National Park (EINP) is located on Hwy #16, 37 km east of the eastern limit of the city of Edmonton at 53°37'N, 112°53'W (Figure l) in the center of a physiographic region known as the Alberta Plain (Lang 1974), On the Alberta Plain are several hills, known as the Beaver Hills, that rise above the level of the surrounding landscape. The bedrock in this area is sedimentary, consisting of non-marine sandstones, siltstones, and mudstones (Emerson 1977).…”
Section: Study Areamentioning
confidence: 99%
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“…Elk Island National Park (EINP) is located on Hwy #16, 37 km east of the eastern limit of the city of Edmonton at 53°37'N, 112°53'W (Figure l) in the center of a physiographic region known as the Alberta Plain (Lang 1974), On the Alberta Plain are several hills, known as the Beaver Hills, that rise above the level of the surrounding landscape. The bedrock in this area is sedimentary, consisting of non-marine sandstones, siltstones, and mudstones (Emerson 1977).…”
Section: Study Areamentioning
confidence: 99%
“…The bedrock in this area is sedimentary, consisting of non-marine sandstones, siltstones, and mudstones (Emerson 1977). Surface materials are composed of glacial tills formed from a hummocky stagnant ice moraine (Lang 1974), giving the area a rugged topography characterized by knobs, kettles, till hummocks, and till ridges (Scace and Associates Ltd. 1976). Prairie mounds are a distinctive feature of the dead-ice moraine, and within the Beaver Hills, these mounds are circular with a basal diameter of about 91 m and a rim that rises 5 m above the surrounding land.…”
Section: Study Areamentioning
confidence: 99%
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“…Research was conducted in Riding Mountain National Park, Manitoba, Canada (Figure 1). The park occupies an area of 2,978 km 2 (1,148 mi 2 ) in western Canada, 225 km northwest from Winnipeg (50.6580uN, 99.9721uW) and consists of large areas of rolling upland (550 to 640 m [1,804 to 2,099 ft]) underlain by glacial tills (Lang 1974). The region is characterized by mean annual precipitation of 450 to 500 mm and a growing season of 168 to 173 d; mean temperatures range between 218 C (0 F) in January and 18 C (64 F) in July (Leeson et al 2005).…”
Section: Methodsmentioning
confidence: 99%