St. Cuthbert's Swallet

Interest in the possible existence of a cave at this location existed before 1927, and increased when St Cuthbert's Pool suddenly drained away in that year. Attempts to discover an entrance took place between 1944 and 1953, when entry was finally gained. Exploration continued to push the known limits of the cave throughout the 1950s and 1960s. Sump 1 was passed in 1969. Sump 2 has not yet been passed.

St Cuthbert's Swallet is a classic example of a deep phreatic cave system developed at a depth of not less than 280 ft beneath the water table. It contains inclined bedding plane mazes at many levels, fault-guided rifts and some significant chambers. Nine successive phases of sediment deposition, stalagmite deposition and stream erosion have been recognised at the site, providing an exceptional record of environmental change through the warm and cold phases of the Ice Age. St. Cuthbert's Swallet is attractive to cavers, for its complexity and size, reaching over 6.7 km and a depth of 145 m, and having numerous large decorated chambers, forming phreatic mazes on seven distinct levels. Among…

Due to a still enforceable court injunction dating from 1863, which required that the stream now known to run through the cave to Wookey Hole was not polluted, the cave is locked and access is controlled by the Bristol Exploration Club on behalf of the landowners. No novices are allowed to enter.