[1][2] It is prominently visible from the Peyto Lake Overlook in Banff National Park.

It was named after Caldron Lake which is 3 km (1.9 mi) from its summit.

Like other mountains in Banff Park, Caldron Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

[6] Temperatures can drop below -20 C with wind chill factors below -30 C. Precipitation runoff from Caldron Peak Peak drains into the Mistaya River which is a tributary of the North Saskatchewan River.

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