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
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Keywords:caton, claughton, dry stone walls, enclosures, glaciation, haylot, hills, ice age, kames, lancashire, littledale, mounds, sheep fold, trees
