Stanley Peak is a 3,155-metre (10,351ft) mountain located in the Ball Range, at the northeastern section of Kootenay National Park, in the Canadian Rocky Mountains (British Columbia, Canada).[3][4] The mountain was named in 1901 by its first climber, the English explorer Edward Whymper, after Frederick Stanley, 16th Earl of Derby, the sixth Governor-General of Canada.[3][4] There are sources that date the naming in 1912 after Stanley H. Mitchell, Secretary-Treasurer of Alpine Club of Canada.[1]
The valley below Stanley Peak and its glacier, taken from the Stanley Glacier Trail
The peak is visible from the Trans-Canada Highway and Highway 93. Stanley Glacier on the northeast face of the peak can be seen up close by following a hiking trail into a hanging valley between the peak and a southern outlier of Storm Mountain.[5]
Stanley Peak can be ascended from a scrambling route by late summer but involves much routefinding among the many ledges and gullies on the north face.[2] Climbing routes (UIAA III) travel the north and northeast faces.
Stanley Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods that was pushed east and over the top of younger rock during the Laramide orogeny.[8]
Climate
Based on the Köppen climate classification, the mountain 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.
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.
Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.
2019-2025 WikiSort.org - проект по пересортировке и дополнению контента Википедии