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Crescent Falls
Crescent Falls is a series of two waterfalls located on the Bighorn River in the Bighorn River Canyon in west-central Alberta, Canada. They were originally called the Bighorn Falls, after the river they are located on. The current name is a reference to the crescent cliff over which they drop. The falls are located a few kilometres upstream of the river's confluence with the North Saskatchewan River. A gravel road leads north from David Thompson Highway (between Abraham Lake and Nordegg) to the falls. The Crescent Falls Provincial Recreation Area is immediately up-river from the falls. The waterfall is two-tiered and has a height of . Visitors are allowed at the waterfalls year-round. The rock ledges around the top of the falls are slippery and fatal drops have occurred. Additionally, people have died by being swept under the waterfall after swimming at the bottom of the falls. Arthur Philemon Coleman, a professor of geology at the University of Toronto, made the first mention ...
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Clearwater County, Alberta
Clearwater County is a municipal district in west central Alberta, Canada in Division No. 9. Its northwest boundary is the Brazeau River. The municipal office is located in the Town of Rocky Mountain House. The county has a land area of 18,691.65 km2 (7,216.89 sq mi) and comprises close to 99% of Census Division No. 9's land area of 18,921.38 km2 (7,305.59 sq mi). Although the territory excluded is rather small in geographical area, it comprises the major population centre of Rocky Mountain House, which has one-third of Division No. 9's population, in addition to the communities of Caroline, Burnstick Lake and three Indian reserves. The county's 2016 census population was 11,947. The economy of the county is based on agriculture, oil and gas and forestry, with tourism increasing in importance in recent years. On July 1, 2000, the name was changed from "Municipal District of Clearwater No. 99" to "Clearwater County". Geography Communities and localities Th ...
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Bighorn River (Alberta)
The Bighorn River is a short river originating in the Alberta foothills, and is a tributary of the North Saskatchewan River. The river, as well as the nearby Bighorn Range and Bighorn Dam are named for the Bighorn sheep which dominate the area. The name first appeared in 1865. Flowing under Mount McGuire, Bighorn River soon takes on Littlehorn and Sunkay Creeks, before plummeting over the impressive Crescent Falls. After the falls, the Bighorn travels through a significant canyon, before passing through the Bighorn Indian Reserve. The river then empties into the North Saskatchewan River after Lake Abraham.Mussio Ventures (2004). ''Southwestern Alberta Backroad Mapbook,'' Burnaby: Mussio Ventures. See also *List of Alberta rivers Alberta's rivers flow towards three different bodies of water, the Arctic Ocean, the Hudson Bay and the Gulf of Mexico. Alberta is located immediately east of the continental divide, so no rivers from Alberta reach the Pacific Ocean. List of riv ...
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Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which Erosion, erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is gen ...
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Central Alberta
Central Alberta is a region located in the Canadian province of Alberta. Central Alberta is the most densely populated rural area in the province. Agriculture and energy are important to the area's economy. Geography Central Alberta is bordered by the Canadian Rockies in the west, Southern Alberta and the Calgary Region to the south, Saskatchewan to the east and Northern Alberta to the north. It completely surrounds the Edmonton Capital Region and contains the central part of the heavily populated Calgary-Edmonton Corridor. The North Saskatchewan River crosses the region from west to east. Other rivers traversing the area are Red Deer River, Battle River, Athabasca River, Pembina River, Brazeau River, Beaver River. Tourist attractions in the region include: Alberta Prairie Railway Excursions, the Canadian Petroleum Discovery Centre in Leduc, Discovery Wildlife Park, Kerry Wood Nature Centre and Gaetz Lake Sanctuary in Red Deer, Nordegg Heritage Centre and Mine Site, Rey ...
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Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ...
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North Saskatchewan River
The North Saskatchewan River is a glacier-fed river that flows from the Canadian Rockies continental divide east to central Saskatchewan, where it joins with the South Saskatchewan River to make up the Saskatchewan River. Its water flows eventually into the Hudson Bay. The Saskatchewan River system is the largest shared between the Canadian provinces of Alberta and Saskatchewan. Its watershed includes most of southern and central Alberta and Saskatchewan. Course The North Saskatchewan River has a length of , and a drainage area of . At its end point at Saskatchewan River Forks it has a mean discharge of . The yearly discharge at the Alberta–Saskatchewan border is more than . The river begins above at the toe of the Saskatchewan Glacier in the Columbia Icefield, and flows southeast through Banff National Park alongside the Icefields Parkway. At the junction of the David Thompson Highway (Highway 11), it initially turns northeast for before switching to a more direct easter ...
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Alberta Highway 11
Alberta Provincial Highway No. 11, commonly referred to as Highway 11 and officially named the David Thompson Highway, is a provincial highway in central Alberta, Canada. It runs for from Highway 93 at Saskatchewan River Crossing near Mount Sarbach in Banff National Park east to Highway 12 near Nevis. It passes by Nordegg and through Rocky Mountain House, Sylvan Lake and Red Deer along its course. The highway is named after David Thompson, a British-Canadian fur trader, surveyor, and map-maker who explored the area between Rocky Mountain House and Kootenae House (near present-day Invermere, British Columbia) through Howse Pass. Route description The majority of Highway 11 is maintained by Alberta Transportation. The segment within Banff National Park is maintained by the Government of Canada, and within Red Deer limits the city has jurisdiction and is responsible for maintenance. It begins at the Icefields Parkway (Highway 93) and travel ...
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Abraham Lake
Abraham Lake, also known as Lake Abraham, is an artificial lake and Alberta's largest reservoir. It is located in the " Kootenay Plains area of the Canadian Rockies' front range", on the North Saskatchewan River in western Alberta, Canada. Description Abraham Lake has a surface area of and a length of . Although man-made, the lake has the blue color of other glacial lakes in the Rocky Mountains, which is caused by rock flour. Abraham Mountain, Elliott Peak, and the Cline River Heliport are located on the western shore of the lake. Mount Michener is situated on the eastern shore. Mount Ernest Ross lies at the southern tip of the lake. History Abraham Lake was created by the former Calgary Power Company, now TransAlta, in 1972, with the construction of the Bighorn Dam. Planning of the dam involved no evaluation of the social and environmental effects it may have caused and no public hearings were held prior to the construction. Construction of the Bighorn Dam flooded the Koote ...
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Nordegg, Alberta
Nordegg is a hamlet in west-central Alberta, Canada within Clearwater County. It is located in the North Saskatchewan River valley in the foothills of the Canadian Rockies, just east of the intersection of the David Thompson Highway and the Highway 734 spur of the Bighorn Highway (the Forestry Trunk Road). A former coal mining town, it was named after Martin Nordegg and the name probably means "North Corner" in a German dialect. The railway station name at the locality was called ''Brazeau'' rather than ''Nordegg'' at certain points in its history, but the local post office has always been named ''Nordegg''. The name ''Brazeau'' is now obsolete. History In 1907, Martin Cohn (who later changed his surname to Nordegg) of the German Development Company, working with D.B. Dowling of the Geological Survey of Canada, staked claims covering coal deposits near the South Brazeau (now Blackstone), Bighorn, and North Saskatchewan rivers. At Nordegg's urging, Brazeau Collieries Ltd. wa ...
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Arthur Philemon Coleman
Arthur Philemon Coleman (April 4, 1852 – February 26, 1939) was a Canadian geologist and academic. Biography Born in Lachute, Quebec, the son of Rev. Francis Coleman and Emmeline Maria Adams, he received his Bachelor of Arts in 1876 and Master of Arts in 1880 from Victoria College in Cobourg, Ontario. He received a Ph.D. at the University of Breslau in 1881. Coleman joined the department of geology and natural history at Victoria College in 1882 as a Professor. From 1891 to 1901, he was a Professor of Geology at the School of Practical Science in Toronto. From 1893 to 1909, he was a geologist at the Bureau of Mines of the Government of Ontario. From 1901 to 1922, he was a Professor of Geology at the University of Toronto and was Dean of the Faculty of Arts from 1919 to 1922. From 1931 to 1934, he was a geologist with the Department of Mines of the Government of Ontario. In 1898, Coleman lead a field expedition with the intent of surveying resources, along with the Geologist ...
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University Of Toronto
The University of Toronto (UToronto or U of T) is a public research university in Toronto, Ontario, Canada, located on the grounds that surround Queen's Park. It was founded by royal charter in 1827 as King's College, the first institution of higher learning in Upper Canada. Originally controlled by the Church of England, the university assumed its present name in 1850 upon becoming a secular institution. As a collegiate university, it comprises eleven colleges each with substantial autonomy on financial and institutional affairs and significant differences in character and history. The university maintains three campuses, the oldest of which, St. George, is located in downtown Toronto. The other two satellite campuses are located in Scarborough and Mississauga. The University of Toronto offers over 700 undergraduate and 200 graduate programs. In all major rankings, the university consistently ranks in the top ten public universities in the world and as the top university ...
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Foothills
Foothills or piedmont are geographically defined as gradual increases in elevation at the base of a mountain range, higher hill range or an upland area. They are a transition zone between plains and low relief hills and the adjacent topographically higher mountains, hills, and uplands. Frequently foothills consist of alluvial fans, coalesced alluvial fans, and dissected plateaus. Description Foothills primarily border mountains, especially those which are reached through low ridges that increase in size closer and closer to the mountain, but can also border uplands and higher hills. Examples Areas where foothills exist, or areas commonly referred to as the foothills, include the: *Sierra Nevada foothills of California, USA *Foothills of the San Gabriel Valley in Los Angeles County, California, USA *Rocky Mountain Foothills in British Columbia and Alberta, Canada *Silesian Foothills in Silesia, Poland *Sivalik Hills along the Himalayas in the Indian subcontinent * Catalin ...
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