Mt. Ball can be ascended from a scrambling route by late summer but involves remote bushwhacking, which limits the number of attempts per year. The trailhead is located at the Marble Canyon Campground in Kootenay National Park.[2]
Geology
Mount Ball 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.[10]
Climate
Based on the Köppen climate classification, Mount Ball is located in a subarctic climate zone with cold, snowy winters, and mild summers.[11] Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports glaciers on its slopes. Precipitation runoff from the east slope drains to the Bow River via Redearth Creek, and the west slope drains into tributaries of the Vermilion River.
Gallery
East aspect of Mount Ball reflected in Shadow Lake
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Thorington, J. Monroe (1966) [1921]. "Simpson Pass to Vermilion Pass". A Climber's Guide to the Rocky Mountains of Canada. With the collaboration of Putnam, William Lowell (6th ed.). American Alpine Club. p. 52. ISBN978-1376169003.