Mount Coleman is a 3,135-metre (10,285 ft) mountain summit located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada.[2] Its nearest higher peak is Cirrus Mountain, 4.46 km (2.77 mi) to the north.[3] Mount Coleman is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass.

Mount Coleman
Mount Coleman (centered in distance) seen from Icefields Parkway
Highest point
Elevation	3,135 m (10,285 ft)[1]
Prominence	775 m (2,543 ft)[1]
Parent peak	Cirrus Mountain (3270 m)[1]
Listing	Mountains of Alberta
Coordinates	52°07′08″N 116°55′17″W[2]
Geography
Mount Coleman Location of Mount Coleman in Alberta Show map of Alberta Mount Coleman Mount Coleman (Canada) Show map of Canada
Location	Alberta, Canada
Parent range	Canadian Rockies
Topo map	NTS 83C2 Cline River[1]
Geology
Type of rock	Sedimentary

History

Mount Coleman was named in 1898 after Arthur P. Coleman (1852-1939), a Canadian geologist and among the first white men to explore the area that is now Jasper National Park.[4]

Geology

Like other mountains in Banff Park, Mount Coleman is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.[5] Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[6]

Climate

Based on the Köppen climate classification, Mount Coleman is located in a subarctic climate with cold, snowy winters, and mild summers.[7] Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Coleman drains into tributaries of the North Saskatchewan River.

Further reading

• Chic Scott, Pushing the Limits: The Story of Canadian Mountaineering, P 70

See also

• Geography of Alberta

References

External links

• Parks Canada web site: Banff National Park

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