Mount Carr | |
Elevation M: | 2590. |
Elevation Ref: | [1] [2] |
Prominence M: | 133 |
Parent Peak: | Castle Towers Mountain |
Isolation Km: | 1.61 |
Etymology: | Pvt. Frank Edward Carr |
Country: | Canada |
Region Type: | Province |
Region: | British Columbia |
Part Type: | Protected area |
Part: | Garibaldi Provincial Park |
District: | New Westminster Land District |
Range: | Garibaldi Ranges Coast Mountains |
Listing: | Mountains of British Columbia |
Map: | British Columbia#Canada |
Label Position: | right |
Mapframe: | yes |
Mapframe-Zoom: | 8 |
Mapframe-Caption: | Interactive map of Mount Carr |
Coordinates: | 49.9242°N -122.9311°W |
Coordinates Ref: | [3] |
First Ascent: | 1911 |
Easiest Route: | via Sphinx Glacier |
Mount Carr is a 2590abbr=offNaNabbr=off mountain summit located in British Columbia, Canada.
Mount Carr is set within Garibaldi Provincial Park and is part of the Garibaldi Ranges of the Coast Mountains.[1] It is situated 700NaN0 north of Vancouver and 20NaN0 south-southeast of line parent Castle Towers Mountain.[1] Precipitation runoff and glacial meltwater from the west side of the peak drains to Garibaldi Lake, and the eastern slope drains to Cheakamus Lake. Topographic relief is significant as the summit rises 1,440 meters (4,724 feet) above Isosceles Creek in 4 kilometers (2.5 miles).
The peak is named after Frank Edward Carr (1886–1915), Vancouver post office clerk and British Columbia Mountaineering Club executive member, who served with the 7th Battalion, Canadian Expeditionary Forces, in Canada, England and France during World War I.[4] He was killed in action April 26, 1915, in France and is commemorated at the Menin Gate Memorial to the Missing in Belgium.[5] The toponym was officially adopted September 2, 1930, by the Geographical Names Board of Canada.[3]
The first ascent of Mt. Carr, which at the time was known as Copper Peak, was made in 1911 by a large BC Mountaineering Club party including Don Munday.[6] [7]
Based on the Köppen climate classification, Mount Carr is located in the marine west coast climate zone of western North America.[8] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Sphinx Glacier on the west slope, Gray Glacier on the east, and the Cheakamus Glacier on the north slope.