Why take your kids to an ordinary playground slide at the park, when you can go to the slide named after the Devil himself? Unfortunately for sliders, Devils Slide is not a real slide, but an unusual geologic feature found in northern Utah.
Devils Slide is a classic example of how different rock layers, depending on their composition, are affected by weathering and erosion.
Devils Slide looking from the south.
Gate in the foreground for scale.
The sides of the slide are hard, weather-resistant limestone layers about 40 feet high, 25 feet apart, and several hundred feet in length. In between these two hard layers is a shaly limestone that is slightly different in composition from the outer limestone layers. This middle layer is softer, which makes it more susceptible to weathering and erosion, thus forming the chute of the slide