Bow Glacier Falls

Bow Glacier Falls is a waterfall in Banff National Park where water drops rapidly over a steep rock face and crashes at the base with considerable force. The water from the falls feeds into streams that eventually flow into the larger river system downstream.

The waterfall came into being as the Bow Glacier retreated from its earlier position, exposing a rock face over which water now flows. This glacier movement shaped the landscape gradually and created the chasm visible today.

The trail passes an inukshuk stone formation at the base, reflecting the traditional navigation markers used by Indigenous peoples in North America.

The hiking trail to the base of the waterfall starts from a mountain lodge and takes about two hours round trip. Good footwear and some preparation are important, especially on warm days when paths can become dry or slippery.

During winter months the water freezes solid and forms massive ice structures that remain intact for several months, reshaping the rock face in a different way. These ice formations attract special attention from photographers and climbers who travel specifically to see this seasonal transformation.