Devils Slide

Devils Slide

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Devils Slide is a prominent geological formation in Weber Canyon, Utah, United States. It consists of two parallel limestone strata, each approximately 25 feet wide and 200 feet high, extending down the mountainside. The formation is located near the Weber River and is a notable geological feature in the region.

More about Devils Slide

Devils Slide was formed during the Jurassic period, primarily composed of limestone, which was tilted and eroded over time, creating the distinct parallel ridges seen today. It is accessible via Interstate 84, with nearby viewpoints for visitors. The site provides insight into geological processes and is a point of interest for both geologists and tourists.