The first ascent of the mountain was made in 1930 by Kate (Katie) Gardiner and Walter Feuz.[3] The duo also made the first ascents of nearby Mount Foch and Mount Lyautey that same year.[7]
Geology
Mount Sarrail is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.[8]
Climate
Based on the Köppen climate classification, Mount Sarrail is located in a subarctic climate with cold, snowy winters, and mild summers.[9] Temperatures can drop below −20 °C with wind chill factors below −30 °C. In terms of favorable weather, June through September are the best months to climb Mount Sarrail. Precipitation runoff from the mountain drains into tributaries of the Kananaskis River.
^Gadd, Ben (2008), Geology of the Rocky Mountains and Columbias
^Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN1027-5606.
Gallery
Upper Kananaski Lake with Mount Sarrail to right
Aerial view of Foch and Sarrail with the Kananaskis Lakes