The form and depth the curious ne'er could prove "Near which are seen the clefts of GINGLING-COVE The next reference appeared in verse in Thomas Dixon's A Description of the Environs of Ingleborough of 1781: The first reference to Jingling Pot was by John Covel (1638-1722) who wrote in a description of his travels that he was "particularly pleased with Gingling Cove and Reeking Cove near Ingleton, which outdoe Oakey Hole in Somersetshire, and all the wonders of the Peak". After a damp 3 metres (9.8 ft) climb down, the passage enters the much larger Rowten Caves. Initially low, and requiring crawling, it gradually increases in height, passing under a couple of windows where the roof has collapsed. Jingling Cave is about 375-metre (1,230 ft) long. Jingling Cave Ī few metres to the north-west of Jingling Pot, the water of Jingling Beck sink into Jingling Cave. The water probably originally flowed through to the One-armed Bandit Series in Aquamole Pot, and thence down to the West Kingsdale main drain. It is formed on what is thought to be a strike-slip fault with minimal displacement by the waters of Jingling Beck, which now bypass the entrance except in exceptionally wet weather. Jingling Pot is a karst cave formed within the Great Scar Limestone Group of the Visean Stage of the Carboniferous Period, laid down about 335 Ma. These can be entered through a rock window a little way below the entrance. A second set of shafts descend parallel to the surface shaft. A narrow shaft in this second chamber drops into a complex of small crawls and rifts, which approach close to a passage in the One-armed Bandit Series of Aquamole Pot. At the bottom the rift extends to the north and descends steeply into a further chamber, at the end of which the initials of the original explorers may be seen scratched into the rock. Located adjacent to Jingling Beck, it is a lenticular-shaped 45-metre (148 ft) deep shaft that descends straight from the surface. Jingling Pot is a limestone cave in West Kingsdale, North Yorkshire, England.
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