Freeman River | |
---|---|
Location | |
Country | Canada |
Province | Alberta |
Physical characteristics | |
Source | |
• location | Freeman River Headwaters |
• coordinates | 54°39′56″N115°57′54″W / 54.66556°N 115.96500°W |
• elevation | 1,096 m (3,596 ft) |
Mouth | |
• location | Athabasca River |
• coordinates | 54°19′14″N114°47′16″W / 54.32056°N 114.78778°W Coordinates: 54°19′14″N114°47′16″W / 54.32056°N 114.78778°W |
• elevation | 605 m (1,985 ft) |
The Freeman River is a short river in west-central Alberta, Canada. The Freeman takes its name from the fur traders, who, after leaving the employ of the Hudson's Bay Company or the North West Company, decided to remain in the interior and work as free trappers or free hunters. [1]
The river flows in a southeastern direction for much of its course. It flows through a significant petroleum and natural gas field near the town of Swan Hills, before being bridged by Alberta Highway 32. The river then runs parallel to Alberta Highway 33, takes on the Morse River, and joins the Athabasca River near Fort Assiniboine.
The Freeman River has experienced significant flooding in the past. Particularly notable is the flood of July 1971, which swept away a bridge crossing the river near Fort Assiniboine, Alberta. One first-year science student from the University of Alberta, who was working with the Provincial Ecology Corps over the summer, was killed when the bridge collapsed and fell into the river. [2]
The Fraser River is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for 1,375 kilometres (854 mi), into the Strait of Georgia just south of the City of Vancouver. It is the 11th longest river in Canada. The river's annual discharge at its mouth is 112 cubic kilometres (27 cu mi) or 3,550 cubic metres per second (125,000 cu ft/s), and it discharges 20 million tons of sediment into the ocean.
The Assiniboine River is a 1,070-kilometre (660 mi) river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle, Souris and Whitesand Rivers. For early history and exploration see Assiniboine River fur trade.
Fish Creek Park is an urban provincial park that preserves the valley of Fish Creek in the southern part of Calgary, Alberta, Canada. It is bordered on three sides by the city, and on the west by the territory of the Tsuu T’ina Nation (Sarcee), a First Nation.
Alberta Provincial Highway No. 2, commonly referred to as Highway 2 or the Queen Elizabeth II Highway, is a major highway in Alberta that stretches from the Canada–United States border through Calgary and Edmonton to Grande Prairie. Running primarily north to south for approximately 1,273 kilometres (791 mi), it is the longest and busiest highway in the province carrying more than 170,000 vehicles per day near Downtown Calgary. The Fort Macleod—Edmonton section forms a portion of the CANAMEX Corridor that links Alaska to Mexico. More than half of Alberta's 4 million residents live in the Calgary–Edmonton Corridor created by Highway 2.
Deerfoot Trail is a 46.4-kilometre (28.8 mi) freeway segment of Highway 2 in Calgary, Alberta, Canada. It stretches the entire length of the city from south to north and links suburbs to downtown via Memorial Drive and 17 Avenue SE. The freeway begins south of Calgary where it splits from Macleod Trail, crosses the Bow River into city limits, and reaches the Stoney Trail ring road. Crisscrossing twice more with the river, it intersects Glenmore Trail and Memorial Drive; the former is a major east–west expressway while the latter is a freeway spur into downtown. In north Calgary, it crosses Highway 1 and passes Calgary International Airport before ending at a second interchange with Stoney Trail. Highway 2 becomes the Queen Elizabeth II Highway as it continues north into Rocky View County towards Edmonton.
The Elbow River is a river in southern Alberta, Canada. It flows from the Canadian Rockies to the city of Calgary, where it merges into the Bow River.
Alberta Provincial Highway No. 3, commonly referred to as Highway 3 and officially named the Crowsnest Highway, is a 324-kilometre (201 mi) highway that traverses southern Alberta, Canada, running from the Crowsnest Pass through Lethbridge to the Trans-Canada Highway in Medicine Hat. Together with British Columbia Highway 3 which begins in Hope, it forms an interprovincial route that serves as an alternate to the Trans-Canada from the Lower Mainland to the Canadian Prairies.
Fort Assiniboine is a hamlet in northwest Alberta, Canada, within Woodlands County. It is located along the north shore of the Athabasca River at the junction of Highway 33 and Highway 661. It is approximately 39 kilometres (24 mi) northwest of Barrhead, 62 kilometres (39 mi) southeast of Swan Hills and 91 kilometres (57 mi) northeast of Whitecourt.
Alberta Provincial Highway No. 8, commonly referred to as Highway 8, is a highway in Southern Alberta that connects Highway 22 in Rocky View County, just north of Redwood Meadows, to Calgary.
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.
Highway 35 is a paved undivided provincial highway in the Canadian province of Saskatchewan. It runs from the US Border near Port of Oungre to a dead end near the north shore of Tobin Lake. Saskatchewan Highway 35 (SK Hwy 35) is about 569 kilometres (354 mi) long. The CanAm Highway comprises Saskatchewan Highways 35, SK Hwy 39, SK Hwy 6, SK Hwy 3, SK Hwy 2 and U.S. Route 85. 74.6 kilometres (46.4 mi) of SK Hwy 35 contribute to the CanAm Highway between Port of Oungre on the Canada – United States border and Weyburn. Mudslides, and spring flooding were huge road building and maintenance problems around Nipawin as well as along the southern portion of the route named the Greater Yellow Grass Marsh. Over 20 early dams were built until the problem was addressed with the Rafferty-Alameda Project on the Souris River and the construction of the Qu'Appelle River Dam which have helped to eliminate washed out roads and flooded communities. The highway through the homesteading community followed the Dominion Land Survey on the square until reaching the Saskatchewan River at Nipawin. The completion of the combined railway and traffic bridge over the Saskatchewan River at Nipawin in the late 1920s retired the ferry and basket crossing for traffic north of Nipawin. The E.B. Campbell Dam built in 1963 northeast of Nipawin created Tobin Lake, and Codette Lake was formed with the construction of the Francois-Finlay Hydroelectric dam at Nipawin. The railway/traffic bridge that formed part of Highway 35 was the only crossing utilized at Nipawin until a new traffic bridge was constructed in 1974. The new bridge then became part of the combined Highway 35 and 55 until the highway parts just east of White Fox. Highway 35 then continued north along the west side of Tobin Lake. The railway/traffic bridge continues to be utilized for one lane vehicle traffic controlled by traffic lights, and continues as the "old highway 35" on the west side of the river until it joins with the current Highway 35/55.
The history of flooding in Canada includes floods caused by snowmelt runoff or freshet flooding, storm-rainfall and "flash flooding", ice jams during ice formation and spring break-up, natural dams, coastal flooding on ocean or lake coasts from storm surges, hurricanes and tsunamis. Urban flooding can be caused by stormwater runoff, riverine flooding and structural failure when engineered flood management structures, including dams and levees, prove inadequate to manage the quantities and force of flood waters. Floods can also occur when groundwater levels rise entering buildings cracks in foundation, floors and basements.(Sandink 2010, p. 7). Flooding is part of the natural environmental process. Flooding along large river systems is more frequent in spring where peak flows are often governed by runoff volume due to rainfall and snowmelt, but can take place in summer with flash floods in urban systems that respond to short-duration, heavy rainfall. Flooding due to hurricanes, or downgraded severe storms, is a concern from August to October when tropical storms can affect Eastern North America. Flood events have had a significant effect on various regions of the country. Flooding is the costliest natural disaster for Canadians. Most home insurance claims in Canada deal with water damage due to sewer back-up, not fire.
The Red Coat Trail is a 1,300-kilometre (810 mi) route that approximates the path taken in 1874 by the North-West Mounted Police in their March West from Fort Dufferin to Fort Whoop-Up.
The Paddle River is a short river in northern Alberta, Canada. Known as Pimiskāw sīpiy by the Cree, the river was named because of its slow speed. During the fur trade era, a canoe could be easily paddled up the river, in contrast to the more arduous task of ascending a swifter river like the Pembina River that required poling or tracking.
The Blindman River is a river in south-central Alberta. It forms south of Winfield, Alberta and flows southeastward before joining the Red Deer River near Red Deer. The Blindman is bridged by Alberta Highway 20 a number of times in its upper reaches, before passing near the town of Rimbey. The river then takes on the outflow of Gull Lake. It is bridged by Alberta Highway 2 at Red Deer before flowing into the Red Deer River.
The Gregg River is a short river in west-central Alberta, Canada. The river is named after John James Gregg (1840–1941), a prospector and trapper prominent in the area.
The Edson River is a minor river in west-central Alberta, Canada. The river, like the nearby town of Edson, is named for Edson Joseph Chamberlin (1852–1924), a Vice-President and General Manager of the Grand Trunk Pacific Railway. Chamberlain also acted as the President of the Grand Trunk Railway.
The Iron Confederacy or Iron Confederation was a political and military alliance of Plains Natives of what is now Western Canada and the northern United States. This confederacy included various individual bands that formed political, hunting and military alliances in defense against common enemies. The ethnic groups that made up the Confederacy were the branches of the Cree that moved onto the Great Plains around 1740, the Saulteaux, the Nakoda or Stoney people also called Pwat or Assiniboine, and the Métis and Haudenosaunee. The Confederacy rose to predominance on the northern Plains during the height of the North American fur trade when they operated as middlemen controlling the flow of European goods, particularly guns and ammunition, to other Indigenous nations, and the flow of furs to the Hudson's Bay Company (HBC) and North West Company (NWC) trading posts. Its peoples later also played a major part in the bison (buffalo) hunt, and the pemmican trade. The decline of the fur trade and the collapse of the bison herds sapped the power of the Confederacy after the 1860s, and it could no longer act as a barrier to U.S. and Canadian expansion.
In the days leading up to June 19, 2013, Alberta, Canada, experienced heavy rainfall that triggered catastrophic flooding described by the provincial government as the worst in Alberta's history. Areas along the Bow, Elbow, Highwood, Red Deer, Sheep, Little Bow, and South Saskatchewan rivers and their tributaries were particularly affected. A total of 32 states of local emergency were declared and 28 emergency operations centres were activated as water levels rose and numerous communities were placed under evacuation orders.
Calgary Trail and Gateway Boulevard are a pair of major arterial roadways in Edmonton, Alberta. Gateway Boulevard carries northbound traffic while Calgary Trail carries southbound traffic. From south of 31 Avenue, they form a two-way freeway separated by a median; for this portion, the roadway maintains the separate names for northbound and southbound traffic. Near 31 Avenue, Calgary Trail and Gateway Boulevard separate and become parallel one-way arterial roadways to Saskatchewan Drive, at the edge of the North Saskatchewan River valley. Designated as part of Highway 2 south of Whitemud Drive, it is Edmonton's main southern entrance and is both a major commuter route, connecting to the Edmonton International Airport and Leduc, as well as a regional connection to Red Deer, and Calgary.
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