Mount Boswell is a 2,454-metre (8,051-foot) summit located in Waterton Lakes National Park, in the Canadian Rockies of Alberta, Canada.

It is situated along the east shore of Waterton Lake, one kilometre north of the Canada–United States border.

[2] Like other mountains in Waterton Lakes National Park, Mount Boswell is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

[6] Based on the Köppen climate classification, Mount Boswell is located in a subarctic climate with cold, snowy winters, and mild summers.

[7] Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Boswell drains into Waterton Lake, thence Waterton River.