An interesting hill on the valley floor. Its origins probably lie at the end of the last Ice Age event and is almost certainly what is known as a Kame mound caused by the surface water of the melting ice depositing its load of sand and gravel into an eroded hole in the ice.
No EXIF information is available
Categories & Keywords
Keywords:caton, claughton, dry stone walls, enclosures, glaciation, haylot, hills, ice age, kames, lancashire, littledale, mounds, sheep fold, trees