Road Castle

The Anglican Church of St Mary Magdelene in Exford, Somerset, England was built in the 15th century. It is a Grade II* listed building.

Exford is a rural village at the centre of Exmoor National Park, 7 miles (11 km) north-west of Dulverton, and 10 miles (16 km) south-west of Minehead, in Somerset, England. Less than a mile away is the hamlet of Lyncombe. Situated on the B3224, the main route across Exmoor, it is a small village on the River Exe with activities including hunting, shooting, fishing and horse riding.The centre of the village surrounds a traditional village green, and is home to a post office, general store, car repair shop, youth hostel and primary school as well as a children's play area. The village is on the route of the Samaritans Way South West and the Celtic Way Exmoor Option.

The Anglican Church of St Andrew in Withypool, Somerset, England was built in late medieval period. It is a Grade II* listed building.

Withypool (formerly Widepolle, Widipol, Withypoole) is a small village and former civil parish, now in the parish of Withypool and Hawkridge, in the Somerset district, in the ceremonial county of Somerset, England, near the centre of Exmoor National Park and close to the border with Devon. The word Withy means "willow". The parish of Withypool and Hawkridge, covers 3,097 hectares (7,653 acres), includes the village of Hawkridge and has a population around 201.Withypool is in the Barle Valley on the River Barle. The village lies on the route of the Two Moors Way and the Celtic Way Exmoor Option. To the southwest of the village lie Withypool Common and Withypool Hill.

The Withypool Bridge is an arch bridge that carries a small road over the River Barle at Withypool in Somerset, England. It is a Grade II* listed building.The red sandstone bridge was built in the 19th century. It replaced an earlier bridge 100 metres (330 ft) upstream of the current site and is therefore shown on some maps as "New Bridge".The bridge was restored in 1866 and again in 1983.

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 18,810 acres (7,610 ha) 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 55 km (34 mi) of the Bristol Channel coast. The total area of the Exmoor National Park is 692.8 km2 (267.5 sq mi), 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 519 metres (1,703 ft) 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.

South Exmoor (grid reference SS880340) is a 3132.7 hectare (7742.3 acre) biological Site of Special Scientific Interest in Devon and Somerset, England, notified in 1992. The site consists of several fragments of land on the south side of Exmoor. In Devon the site includes Barcombe Down and North Molton Ridge, southeast of South Radworthy, Molland Common, north of Molland, and West Ansty and East Ansty Commons. In Somerset the site includes Brightworthy Barrows and part of Withypool Common, Winsford Hill and Haddon Hill, all within the Exmoor National Park. The site contains extensive areas of heathland including lowland communities which are only found in South West England and South Wales. The River Barle and its tributaries flow through parts of the site and submerged plants such as alternate watermilfoil (Myriophyllum alterniflorum) are abundant. There are small areas of semi-natural woodland within the site, including some which are ancient. The most abundant tree species is sessile oak (Quercus petraea), the shrub layer is very sparse and the ground flora includes bracken, bilberry and a variety of mosses. The heaths have strong breeding populations of whinchat (Saxicola rubetra) and European stonechat (Saxicola rubicola). northern wheatear (Oenanthe oenanthe) are common near stone boundary walls and other stony places. Grasshopper warbler (Locustella naevia) breed in scrub and tall heath. Trees on the moorland edges provide nesting sites for common redpoll (Acanthis flammea), common buzzard (Buteo buteo) and common raven (Corvus corax).

Withypool Stone Circle, also known as Withypool Hill Stone Circle, is a stone circle located on the Exmoor moorland, near the village of Withypool in the southwestern English county of Somerset. The ring is part of a tradition of stone circle construction that spread throughout much of Britain, Ireland, and Brittany during the Late Neolithic and Early Bronze Age, over a period between 3300 and 900 BCE. The purpose of such monuments is unknown, although archaeologists speculate that the stones represented supernatural entities for the circle's builders. Many monuments were built in Exmoor during the Bronze Age, but only two stone circles survive in this area: the other is Porlock Stone Circle. The Withypool ring is located on the south-western slope of Withypool Hill, on an area of heathland. It is about 36.4 metres (119 feet 5 inches) in diameter. Around thirty small gritstones remain, although there may originally have been around 100; there are conspicuous gaps on the northern and western sides of the monument. The site was rediscovered in 1898 and surveyed by the archaeologist Harold St George Gray in 1905.

Almsworthy Common is a small area of unenclosed land in Exmoor, south-western England. It contains a number of archaeological sites. It is about 2 miles north of Exford roughly 0.5 km2 in area, and the Macmillan Way West passes through it, as does the parish boundary between Exford and Porlock. It reaches a height of 453 metres.Stone settings are arrangements of upright stones either scattered randomly or in a roughly geometric pattern. They are the most common form of stone monument found on Exmoor, with 57 conclusively recorded examples in this area. A large number are known to have existed but have been destroyed.560 m south west of Chetsford Bridge is a stone alignment. The archaeologist Aubrey Burl stated that an "eye of faith" was needed to identify "either a ring or a set of rows." The Ordnance Survey list it as a "Stone Circle" on their map. In his 1970 study of the archaeology of Exmoor, Leslie Grinsell thought that it was "probably" a stone circle.The common is also the site of one of the best preserved hut circles on Exmoor.

The Tarr Steps is a clapper bridge across the River Barle in the Exmoor National Park, Somerset, England. They are located in a national nature reserve about 2.5 miles (4 km) south east of Withypool and 4 miles (6 km) north west of Dulverton. A typical clapper bridge construction, the bridge's listing assesses it as medieval in origin. The stone slabs weigh up to two tons each. The bridge is 180 feet (55 m) long and has 17 spans. It has been designated as a Grade I listed building and scheduled monument.

Dunkery Beacon at the summit of Dunkery Hill is the highest point on Exmoor and in Somerset, England. It is also the highest point in southern England outside of Dartmoor. The sandstone hill rises to 519 metres (1,703 ft) and provides views over the surrounding moorland, the Bristol Channel and hills up to 86 miles (138 km) away. The site has been visited by humans since the Bronze Age, and contains several burial mounds in the form of cairns and bowl barrows. Sweetworthy on the lower slopes is the site of two Iron Age hill forts or enclosures and a deserted medieval settlement. The hill is part of a Site of Special Scientific Interest and National nature reserve. It was in private ownership until the 20th century, when it was donated to the National Trust by Sir Thomas Acland, Colonel Wiggin and Allan Hughes; a stone cairn was erected at the summit to commemorate the event.

The Caratacus Stone, sometimes known as the Caractacus Stone, is an inscribed stone on Exmoor in Somerset, England. It is thought to date from the 6th century, and it has been a scheduled monument since 1925.The inscription, in Latin, appears to read CARAACI NEPVS, though experts have stated that a bar above the second A forms a ligature meaning that it should be read as CARATACI NEPVS. It is possible that there was more text on the stone that has weathered away.The inscription, which can be translated as "grandson or immediate descendant of Caratacus", has led to the general opinion that the stone was probably erected as a memorial to a person who claimed the first-century British chieftain Caratacus as an ancestor.The first mention of the stone was in 1219, when it was described in a perambulation of the Royal Forest of Exmoor as "the Langeston". In 1890 the letter N (which is reversed) was missing from the inscription, but by 1919 the missing piece had been found and was cemented back in place. In 1906 a shelter was erected over the stone, and an excavation in 1937 revealed that the stone was not associated with a burial site.