Old Goat Mountain is a 3,120-metre (10,240 ft) mountain summit located in Kananaskis Country in the Canadian Rockies of Alberta, Canada. The mountain is situated near the south end of the Goat Range along the west shore of Spray Lakes Reservoir, and is the highest point in the Goat Range.[2] The east flank of the mountain is within Spray Valley Provincial Park, while the west aspect is within Banff National Park, with the boundary line between the two parks running roughly north-to-south over its summit. The nearest higher peak is Wind Mountain, 8.9 km (5.5 mi) to the east.[1] Old Goat Mountain can be seen from Alberta Highway 742, the Smith-Dorrien/Spray Trail.
Old Goat Mountain | |
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![]() Old Goat Mountain (right) with Mount Nestor (left) | |
Highest point | |
Elevation | 3,120 m (10,240 ft)[1] |
Prominence | 1,444 m (4,738 ft)[1] |
Parent peak | Wind Mountain (3153 m)[1] |
Listing | Mountains of Alberta |
Coordinates | 50°56′40″N 115°22′21″W[1] |
Geography | |
![]() ![]() Old Goat Mountain Location of Old Goat Mountain in Alberta Show map of Alberta![]() ![]() Old Goat Mountain Old Goat Mountain (Canada) Show map of Canada | |
Location | Alberta, Canada |
Parent range | Goat Range, Canadian Rockies |
Topo map | NTS 82J14 Spray Lakes Reservoir[1] |
Geology | |
Age of rock | Cambrian |
Type of rock | Sedimentary |
Climbing | |
Easiest route | Scramble |
The mountain was named "Old Goat" in memory of Rick Collier, a founding member of the Old Goats Climbing Club, who had climbed this peak numerous times and had written much about it.[1] Collier died in a 2012 mountaineering accident,[3] so the mountain's name is not yet official.
Old Goat Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.[4] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[5]
Based on the Köppen climate classification, Old Goat Mountain is located in a subarctic climate with cold, snowy winters, and mild summers.[6] Temperatures can drop below −20 °C (−4 °F) with wind chill factors below −30 °C (−22 °F). Precipitation runoff from the mountain drains into the Spray Lakes Reservoir.
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