Concept

Exmoor

Summary
Exmoor is loosely defined as an area of hilly open moorland in west Somerset and north Devon in South West England. It is named after the River Exe, the source of which is situated in the centre of the area, two miles north-west of Simonsbath. Exmoor is more precisely defined as the area of the former ancient royal hunting forest, also called Exmoor, which was officially surveyed 1815–1818 as in extent. The moor has given its name to a National Park, which includes the Brendon Hills, the East Lyn Valley, the Vale of Porlock and of the Bristol Channel coast. The total area of the Exmoor National Park is , of which 71% is in Somerset and 29% in Devon. The upland area is underlain by sedimentary rocks dating from the Devonian and early Carboniferous periods with Triassic and Jurassic age rocks on lower slopes. Where these reach the coast, cliffs are formed which are cut with ravines and waterfalls. It was recognised as a heritage coast in 1991. The highest point on Exmoor is Dunkery Beacon; at it is also the highest point in Somerset. The terrain supports lowland heath communities, ancient woodland and blanket mire which provide habitats for scarce flora and fauna. There have also been reports of the Beast of Exmoor, a cryptozoological cat roaming Exmoor. Several areas have been designated as Nature Conservation Review and Geological Conservation Review sites. There is evidence of human occupation from the Mesolithic. This developed for agriculture and extraction of mineral ores into the Bronze and Iron Ages. The remains of standing stones, cairns and bridges can still be identified. The royal forest was granted a charter in the 13th century, however foresters who managed the area were identified in the Domesday Book. In the Middle Ages sheep farming was common with a system of agistment licensing the grazing of livestock as the Inclosure Acts divided up the land. The area is now used for a range of recreational purposes. Exmoor has been designated as a national character area (No.
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