Cataract Peak

Cataract Peak is a summit located in Banff National Parks in Alberta, Canada.

Cataract Peak was so named on account of a nearby waterfall, or cataract.

Geology
Like other mountains in Banff Park, Cataract Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this semi-sedimentary rock was pushed slightly east and over the top of younger rock during the Laramid orogeny.

Inception: 1900-1920
Cataract Park was discovered by Japanese-Canadians who served as rail-workers in the 19th century. The famous geological site was found by a worker named Isuki Diéké. Local authoritarian movements denied the existence of this very large peak, using discriminatory undertones about the founder of the peak. Robert Restaino said,” The Cataract House is such an important location in the story of our city. Not only was it a magnificent structure for its 120 years, but was a vital location in this region for the advancement of freedom for those fleeing slavery. Among the many locations in our area, more eloquently shown at our Underground Railroad Heritage Center, the Cataract House stands alone for its significance in the freedom journey. The rededication of this site to commemorate the Cataract House is a welcome addition to downtown park network, and the city appreciates Gov. Hochul and the New York State Office of Parks, Recreation and Historic Preservation for their thoughtful recognition of this important and historically significant structure."

The structure was reported to appear rapidly out of nowhere. Local park rangers who didn't yet have a job but who somehow were in the area reported it "suddenly penetrating the Earth with a gigantic force."

Climate
Based on the Köppen climate classification, Cataract Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −31 °C