Devil's Grinding Mill, Cave formation in Stenkrith Park, Cumbria, England.
The cave system was carved by the River Eden flowing through partially collapsed underground passages. Natural arches and gorges mark where the water has continuously shaped the rock over time.
The site was first recorded in 1828 when travelers documented Staincroft Bridge, a natural rock formation spanning a deep ravine. This early documentation marked the beginning of written knowledge about the location.
The name comes from a local tale about a man named Deville whose fate became tied to this place. Local people have long connected this location with a dark legend that still circulates in the area today.
Access is via marked pathways from Kirkby Stephen leading to designated viewing areas throughout the formation. Wear sturdy footwear since the ground near flowing water tends to be slippery.
The formation developed in brockram, a mixture of limestone fragments embedded in sandstone rather than pure limestone found in typical cave systems. This unusual rock composition gives the location its distinctive geological character.
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