Devil's Slide is a geological formation located in northern Utah's Weber Canyon, approximately 26 miles west of the Wyoming border, near the community of Croydon in Morgan County, Utah, United States. The Slide consists of two parallel limestone strata that have tilted to lie vertical, protruding 40 feet (12 m) out of the mountainside.
Intervening layers have eroded more quickly, forming a channel running hundreds of feet down the mountain. The distance between the two slabs is around 25 feet (7.6 m).
Devil's Slide is a geological formation located in northern Utah's Weber Canyon, approximately 26 miles west of the Wyoming border, near the community of Croydon in Morgan County, Utah, United States. The Slide consists of two parallel limestone strata that have tilted to lie vertical, protruding 40 feet (12 m) out of the mountainside.
Source-backed
Check current access, opening rules, and local transport before adding this stop to an itinerary.
Verify locally
Travelpedia hidden-gem signal
5Devil's Slide (Utah) is mapped from 3 source signal(s) and destination coordinates.