Doughnut Falls, Mountain waterfall in Big Cottonwood Canyon, United States.
Doughnut Falls is a waterfall in Big Cottonwood Canyon where water plunges through a distinctive circular rock opening into a pool below. The natural hole in the stone formation creates an unusual visual effect that changes throughout the seasons.
The waterfall became part of the Wasatch-Cache National Forest trail system as the region developed its hiking network during the mid-20th century. The rock formation itself was shaped by natural geological processes over thousands of years.
Local families and youth groups gather at this waterfall throughout summer months, maintaining a tradition of outdoor recreation in Utah's mountain areas.
The waterfall is reached via a hiking trail that takes two to three hours round-trip with moderate uphill walking. Parking at the trailhead is limited, so arriving early is advisable, especially on weekends.
During winter months the water freezes into ice columns that resemble natural sculptures, completely transforming the site's appearance. These frozen formations occur only under specific weather conditions and attract photographers.
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