Tonsa, or Tonsa Peak, is a mountain summit located on the border of Alberta and British Columbia on the Continental Divide in the Canadian Rockies. The mountain forms part of the backdrop to Moraine Lake in the Valley of the Ten Peaks of Banff National Park. It was named in 1894 by Samuel E.S. Allen for the Stoney Indian word for the number four.
Like other mountains in Banff Park, Tonsa 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.
Based on the Köppen climate classification, Tonsa Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below âÂÂ20 ðC with wind chill factors below âÂÂ30 ðC. Precipitation runoff from Tonsa Peak drains east into tributaries of the Bow River, or west into tributaries of the Vermilion River.
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