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Redgate Crack is a fissure or crack in a rocky outcrop on the hillside above the village of Foolow, near Chapel-en-le-Frith. The crack is about 15 meters (49 feet) long and runs roughly north-south through a gritstone outcrop. The site has garnered attention due to its unusual geological formation, its role in local folklore, and its inclusion in various hiking and exploration activities.

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The name "Redgate" likely refers to the reddish hue of the rocks in the area, which are characteristic of the Carboniferous age gritstones found throughout much of the Peak District. These rocks were formed from sand deposited in a ancient river system that flowed across the area over 300 million years ago. While it may seem counterintuitive, some users choose

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