Floe Peak is a 3,006-metre (9,862 ft) mountain summit located on the western border of Kootenay National Park, in the Canadian Rockies of British Columbia, Canada.

The mountain is part of what is known as the Rockwall in the Vermilion Range, and is named for Floe Lake[4] which is situated below the enormous northern cliffs of the peak.

Floe Peak is composed of limestone, a sedimentary rock laid down during the Precambrian to Jurassic periods and pushed east and over the top of younger rock during the Laramide orogeny.

[5] Based on the Köppen climate classification, Floe Peak is located in a subarctic climate with cold, snowy winters, and mild summers.

Precipitation runoff from the mountain drains east into Floe Creek, a tributary of the Vermilion River, or west into tributaries of the Kootenay River.