In reply to Eskdale massive:
getting there:
Occasionally, hollows are created on the surface of limestone. They form where drift material falls into joints which have been enlarged and widened by chemical solution. The hollows are called dolines or shake holes.
The shake hole is then eroded by streams and a vertical hole known as a pothole or swallow hole is formed. These holes can, in turn, be enlarged by heavy rainfall or glacial meltw*ter. Gaping Gill, in the Yorkshire Dales, is an example of an enlarged swallow hole.
all we need now is sink holes . . .