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.
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.
Gallery
The valley below Stanley Peak and its glacier, taken from the Stanley Glacier Trail
^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.