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300406-14. © NRT, 2006
By Gaping Gill, Ingleborough, Yorkshire Dales National Park, N.Yorks., UK, 30 April, 2006

In addition to the intense solutional erosion by streams, the limestone is more gradually weathered by rainfall. Such small-scale erosion and adjacent redeposition gradually creates surface structures such as those visible on the side of this exposure. The tops have been smoothed by seasonal floods and the passage of human visitors.

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