Bow Valley Provincial Park

Last updated

Bow Valley Provincial Park
Middle Lake in Bow Valley Provincial Park.jpg
Mount Yamnuska seen from Middle Lake in Bow Valley Provincial Park
Kananaskis park system.png
Red pog.svg
Location of Bow Valley Park in Kananaskis Country
Location District of Bighorn No. 8
Flag of Alberta.svg  Alberta Flag of Canada (Pantone).svg  Canada
Nearest city Canmore
Coordinates 51°04′31″N115°04′09″W / 51.07528°N 115.06917°W / 51.07528; -115.06917
Area32.87 km2 (12.69 sq mi)
EstablishedJuly 27, 1959
Governing body Alberta Tourism, Parks and Recreation,
Bow Valley Park Campgrounds

Bow Valley Provincial Park is a provincial park in Alberta, Canada. Established in 1959 in the arch of the Bow River at its confluence with the Kananaskis River, the park is one park of many within the Kananaskis Country park system.

Contents

This park is located at the eastern edge of Alberta's Rocky Mountains in the Bow Valley, and it features trout fishing in the Bow River and spectacular mountain scenery. It includes forested areas, meadows, lakes, and an area of unusual "warm" springs. There are also glacial landforms such as eskers, kames, moraines, and kettle lakes that formed during the retreat of the Bow Valley glacier in the late Pleistocene.

Geologic setting

Entering Bow Valley Provincial Park BowValleyProvincialParkEntrance.jpg
Entering Bow Valley Provincial Park
Mountain scenery at Middle Lake in Bow Valley Provincial Park The Canadian Rockies at Middle Lake, Alberta.jpg
Mountain scenery at Middle Lake in Bow Valley Provincial Park
A trail follows the top of an esker in Bow Valley Provincial Park A trail follows the top of an esker.jpg
A trail follows the top of an esker in Bow Valley Provincial Park

The spectacular mountains that flank the park, such as Mount Yamnuska, consist of resistant Cambrian to Devonian age carbonate rocks that have been placed on top of softer Late Cretaceous sandstones and shales by the McConnell Thrust Fault. That fault also provides a conduit for some of the spring water that surfaces in the Many Springs area of the park. [1]

The spring water at Many Springs has a year-round temperature of about 7 °C (40 °F) and does not freeze in the winter. It originates as precipitation in the surrounding mountains and percolates down to a depth of about 600 m (2,000 ft) where it is warmed by geothermal heat. It then circulates up along the plane of the McConnell Thrust, which passes under the park beneath Many Springs. After mixing with water from the sand and gravel deposits that underlie the Bow Valley, the spring water flows into the lake at a rate of about 100 L/sec (26 gal/sec). [1] [2]

The park also features good examples of fluvioglacial landforms that formed during the retreat of the Bow River valley glacier in the late Pleistocene. [3] These include Middle Lake, which is a kettle lake that was formed by a large block of ice that had become detached from the retreating glacier. The block became surrounded by glacial outwash, and when it melted it left the depression that now holds the lake. [1] [4] There is also a variety of kames, eskers and moraines in the park. [4]

Flora and fauna

After the glacier retreated, the park area was colonized by shrubby pioneer plants that were subsequently replaced by a coniferous forest. [5] The vegetation in the park today is a mix of forested areas and open meadows, and is adapted to cold winters, strong Chinook winds, and hot dry summers. [4]

The forest is dominated by pines and includes spruce, fir, and poplars. Due to strong winds from the west, trees exposed on the tops of ridges commonly lean to the east and lack branches on the windward side. Drier areas of the park are covered by grasses, a wide variety of wildflowers, and low, mat-like juniper shrubs ( Juniperus horizontalis ). Consistently damp, humid areas like Many Springs host moisture-loving plants like yellow lady's slipper ( Cypripedium parviflorum ), butterwort ( Pinguicula vulgaris ), and elephant's head ( Pedicularis groenlandica ). [4]

Because of the relatively warm water from the springs, the lake at Many Springs does not freeze completely in winter, which makes it attractive to beavers and other animals. Animals are also attracted by the sodium chloride in the spring water that creates salt licks for them. The small blind aquatic isopod Salmasellus steganothrix, which is usually found in caves, [6] lives under rocks in the lake at Many Springs. [4]

Bow Valley Wildland Provincial Park

A much larger area, the Bow Valley Wildland Provincial Park, contains the 575 km2 Yamnuska Natural Area that protects the sub-alpine ecosystem of the foothills of the Canadian Rocky Mountains between the Kananaskis park system and Banff National Park, which it borders to the west. [7]

Activities

The following activities are available in the park: [8]

See also

Related Research Articles

<span class="mw-page-title-main">Banff National Park</span> National park in Alberta, Canada

Banff National Park is Canada's oldest national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.

<span class="mw-page-title-main">Canadian Rocky Mountain Parks World Heritage Site</span> Group of national and provincial parks in Canada

The Canadian Rocky Mountain Parks World Heritage Site is located in the Canadian Rockies. It consists of seven contiguous parks including four national parks:

<span class="mw-page-title-main">Kananaskis Country</span> Multiple use area west of Calgary, Alberta, Canada

Kananaskis Country is a multi-use area west of Calgary, Alberta, Canada in the foothills and front ranges of the Canadian Rockies. The area is named for the Kananaskis River, which was named by John Palliser in 1858 after a Cree acquaintance. Covering an area of approximately 4,000 km2 (1,500 sq mi), Kananaskis Country was formed by the Alberta Government in 1978 to provide an assortment of land uses and designations. Land uses include resource extraction activities, recreation, power generation, and residential communities. Land designations include public land and protected areas.

<span class="mw-page-title-main">Bow River</span> River in Alberta, Canada

The Bow River is a river in Alberta, Canada. It begins within the Canadian Rocky Mountains and winds through the Alberta foothills onto the prairies, where it meets the Oldman River, the two then forming the South Saskatchewan River. These waters ultimately flow through the Nelson River into Hudson Bay. The Bow River runs through the city of Calgary, taking in the Elbow River at the historic site of Fort Calgary near downtown. The Bow River pathway, developed along the river's banks, is considered a part of Calgary's self-image.

<span class="mw-page-title-main">Kame</span> Mound formed on a retreating glacier and deposited on land

A kame, or knob, is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier. Kames are often associated with kettles, and this is referred to as kame and kettle or knob and kettle topography. The word kame is a variant of comb, which has the meaning "crest" among others. The geological term was introduced by Thomas Jamieson in 1874.

<span class="mw-page-title-main">The Three Sisters (Alberta)</span> Trio of mountains in Alberta, Canada

The Three Sisters are a trio of peaks near Canmore, Alberta, Canada. They are known individually as Big Sister, Middle Sister and Little Sister.

Alberta Provincial Highway No. 1, commonly referred to as Highway 1, is a major east–west highway in Southern Alberta that forms the southern mainline of the Trans-Canada Highway. It runs from the British Columbia border near Lake Louise through Calgary to the Saskatchewan border east of Medicine Hat. It continues as Highway 1 into both provinces. It spans approximately 534 km (332 mi) from Alberta's border with British Columbia in the west to its border with Saskatchewan in the east. The route is a divided 4-lane expressway throughout the province with the exception of a section in central Calgary where it is an arterial thoroughfare and Urban Boulevard carrying 4 to 6 lanes. The highway is a freeway between the Sunshine exit near the town of Banff and Home Road in Calgary. Other rural sections have at grade intersections with Interchanges only at busier junctions. Twinning of the final 8.5 km (5.3 mi) of Highway 1 between Lake Louise and the British Columbia border was completed by Parks Canada and opened to traffic on June 12, 2014 making the whole length of Alberta Highway 1 a divided minimum 4-lane route.

<span class="mw-page-title-main">Bow Valley</span> Valley in Alberta, Canada

Bow Valley is a valley located along the upper Bow River in Alberta, Canada.

<span class="mw-page-title-main">Tourism in Alberta</span> Tourism in Alberta, Canada

Alberta has been a tourist destination since the early days of the 20th Century, with attractions including national parks, National Historic Sites of Canada, urban arts and cultural facilities, outdoor locales for skiing, hiking and camping, shopping locales such as West Edmonton Mall, outdoor festivals, professional athletic events, international sporting competitions such as the Commonwealth Games and Olympic Winter Games, as well as more eclectic attractions.

<span class="mw-page-title-main">Bow Glacier</span> Glacier in Canada

Bow Glacier is located in Banff National Park, Alberta, Canada, approximately 37 km (23 mi) northwest of Lake Louise. It can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide, and runoff from the glacier supplies water to Bow Lake and the Bow River. The glacier is credited for creating the Bow Valley before retreating at the end of the last glacial maximum.

<span class="mw-page-title-main">Spray Valley Provincial Park</span> Canadian provincial park

Spray Valley Provincial Park is a provincial park located east of the Rocky Mountains, along the Spray River in western Alberta, Canada.

<span class="mw-page-title-main">Kananaskis River</span> River in Alberta, Canada

The Kananaskis River is a mountain river in western Alberta, Canada. It is a tributary of the Bow River, crossing the length of Kananaskis Country.

<span class="mw-page-title-main">Sims Corner Eskers and Kames</span>

Sims Corner Eskers and Kames National Natural Landmark of Douglas County, Washington and nearby McNeil Canyon Haystack Rocks and Boulder Park natural landmarks contain excellent examples of Pleistocene glacial landforms. Sims Corner Eskers and Kames National Natural Landmark includes classic examples of ice stagnation landforms such as glacial erratics, terminal moraines, eskers, and kames. It is located on the Waterville Plateau of the Columbia Plateau in north central Washington state in the United States.

<span class="mw-page-title-main">Alberta's Rockies</span> Rocky Mountains in Alberta, Canada

Alberta's Rockies comprise the Canadian Rocky Mountains in Alberta, Canada. On the southwestern part of the province along the British Columbia border, the region covers all but the south of Census Division 15.

Fluvioglacial landforms are those that result from the associated erosion and deposition of sediments caused by glacial meltwater. These landforms may also be referred to as glaciofluvial in nature. Glaciers contain suspended sediment loads, much of which is initially picked up from the underlying landmass. Landforms are shaped by glacial erosion through processes such as glacial quarrying, abrasion, and meltwater. Glacial meltwater contributes to the erosion of bedrock through both mechanical and chemical processes.

<span class="mw-page-title-main">Spray Lakes Reservoir</span> Reservoir in Kananaskis, Alberta

Spray Lakes Reservoir is a reservoir in Alberta, Canada. The Spray Lakes were a string of lakes formed along the Spray River, a tributary of the Bow River. With the damming of the river, the lakes were united in the Spray Lakes Reservoir.

<span class="mw-page-title-main">Yamnuska Mountain Adventures</span> Mountaineering school & adventure company

Yamnuska Mountain Adventures is a mountaineering school and mountain adventure company located in Canmore, Alberta, Canada. The company was founded in 1975.

The Rocky Mountains Forest Reserve is a tract of land owned by the government of Canadian province of Alberta along the eastern slopes and foothills of the Albertan section of the Canadian Rockies. It is a long strip of land just east of the more famous Canadian Rocky Mountain parks, which is managed for forest and water conservation, public recreation, and industrial goals, rather than aesthetic and preservation goals as in the rocky mountain parks. Forest reserves were established for "...(1) the reserving of timber supplies, (2) the reserving of areas unsuited to agriculture so that they would not be homesteaded, and (3) the preserving of the water level in streams by conserving the timber on the upper watersheds." Government of Canada (1911). “All forest reserves are set aside and constituted for the conservation of the forests and other vegetation in the forests and for the maintenance of conditions favourable to an optimum water supply in those reserves.” Province of Alberta (2004)

Don Getty Wildland Provincial Park is a wildland provincial park in Kananaskis Country, Alberta, Canada. It was created on 24 July 2001 and has an area of 62,775 hectares. The park was named for the 11th premier of Alberta, Don Getty. The park was designated as part of the Special Places 2000: Alberta’s Natural Heritage initiative.

References

  1. 1 2 3 Leckie, D.A. 2017. Rocks, ridges, and rivers - Geologic wonders of Banff, Yoho, and Jasper National Parks, p. 40-44. Broken Poplars, Calgary, 217 p. ISBN   978-0-9959082-0-8.
  2. Toop, D.C. and de la Cruz, N.N. 2002. Hydrogeology of the Canmore corridor and Kananaskis Country, Alberta, p. 4-5 to 4-7. Alberta Environment, Hydrogeology Section, Edmonton, Alberta; report to Western Economic Partnership Agreement, Western Economic Diversification Canada, 83 p.
  3. Rutter, N.W. 1972. Geomorphology and multiple glaciation in the area of Banff, Alberta, p. 22-23. Geological Survey of Canada, Bulletin 206, 54 p.
  4. 1 2 3 4 5 Daffern, G. 2003. Short walks for inquiring minds: Canmore & Kananaskis Country, 2nd edition, p. 55-77. Rocky Mountain Books, Surrey, British Columbia, 296 p. ISBN   978-1-894765-41-1.
  5. Macdonald, G.M. (January 1982). "Late Quaternary paleoenvironments of the Morley Flats and Kananaskis Valley of southwestern Alberta". Canadian Journal of Earth Sciences. 19 (1): 23–35. doi:10.1139/e82-003.
  6. Anonymous. "A cave obligate isopod - Salmasellus steganothrix". Montana Field Guides. Montana Government. Retrieved 3 February 2020.
  7. Alberta Community Development - Kananaskis Country - Bow Valley WP Wildland Park Archived October 6, 2006, at the Wayback Machine
  8. "Activities in Bow Valley Provincial Park". Alberta Tourism, Parks, Recreation & Culture. Retrieved 22 July 2007.[ permanent dead link ]