Timberscombe

Cutcombe is a village and civil parish 9 miles (14 km) south of Minehead and north of Dulverton straddling the ridge between Exmoor and the Brendon Hills in Somerset. It has a population of 361.The parish includes the hamlet of Wheddon Cross which is one of the higher hamlets within the Exmoor National Park at 980 feet (299 m) above sea level, the highest being Simonsbath.

The Anglican Church of St John in Cutcombe, Somerset, England was built in the 13th and 14th centuries. It is a Grade II* listed building.

The Brendon Hills are a range of hills in west Somerset, England. The hills merge level into the eastern side of Exmoor and are included within the Exmoor National Park. The highest point of the range is Lype Hill at 1,388 feet (423 m) above sea level with a secondary summit several kilometres to the southeast at 1,350 feet (411 m). Both points are marked by Ordnance Survey trig points and are located within enclosed farmland. Early versions of the name include Brunedun and Brundon reflecting an original name of Bruna or Brune, meaning 'brown one'. Dun is a common Old English word for a fairly flat and extensive hill. This name is not connected with the village of Brendon in Devon, the name of which has a different origin.The terrain is broken by a series of deeply incised streams and rivers running roughly southwards to meet the River Haddeo, a tributary of the River Exe. The hills are quite heavily cultivated unlike their neighbouring upland areas of Exmoor and the Quantock Hills. The Brendon Hills are largely formed from the Morte Slates, a thick faulted and folded sequence of Devonian age sedimentary rocks. An east-west aligned anticline/syncline pair known as the Brendon Anticline and Brendon Syncline folds these rocks. The fold couplet is itself offset by displacement of the rocks on the NNW-SSE aligned Timberscombe Fault System. Over the centuries they have been mined for minerals, notably ironstone from which iron is extracted for making steel. During the 19th century this activity reached a peak with the West Somerset Mineral Railway, including an 800 feet (244 m) incline, being built to take the ore to Watchet from where it was sent to Ebbw Vale for smelting. The main mining operations ended when the mines were worked out towards the end of the 19th century. The hills are on the route of the Coleridge Way and are also crossed by the Samaritans Way.

Garratts Wood is a woodland in Somerset, England, near the village of Winsford. It covers a total area of 1.11 hectares (2.74 acres). It is owned and managed by the Woodland Trust.

The Anglican St Peter's Church at Exton within the English county of Somerset has a 13th-century tower and 15th century aisle. It is a Grade II* listed building.Some of the original Norman stonework can still be identified in the nave. The rest of the building has been reconstructed with the crenellated two-stage tower being added in the 13th century and the aisle in the 15th. It was restored and the chancel rebuilt in 1876.In the churchyard is a 14th-century cross with a tapering octagonal stone shaft. The upper part of the shaft was restored in 1875.The parish is within the Exmoor benefice and the archdeaconry of Taunton.

Winsford is a village and civil parish in Somerset, England, located about 5 miles (8 km) north-west of Dulverton. It is within the borders of the Exmoor National Park and around 10 miles (16.1 km) south-west of the coastal town of Minehead. The village has one hotel, The Royal Oak dating to before the start of the 16th century, and one shop and post office. There is also a tea garden and a service station, which does not serve fuel for motor vehicles. The village is on the route of the Samaritans Way South West and is located within the Exmoor National Park, to the east of the village is the hamlet of West Howetown.

Exton is a village and civil parish 5 miles (8 km) north-east of Dulverton and 9 miles (14 km) south-west of Dunster in Somerset, England. It lies on the River Exe on Exmoor. The parish includes the village of Bridgetown and covers 2,017 ha, all of which is within the national park.

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.

Sweetworthy is the site of two Iron Age hill forts or enclosures at Luccombe, 4 kilometres (2 mi) south of Porlock, Somerset, England. They are on the north-facing slope of Dunkery Hill. One has a single rampart and external ditch, enclosing 0.25 hectares (0.62 acres). The rampart is still visible and the ditch on the east side is used as a trackway. There was a defended settlement above the main site.It is also the site of a deserted medieval settlement, which has been designated as a scheduled monument. It has been added to the Heritage at Risk Register because of the vulnerability to plant growth.

Gupworthy (sometimes referred to as "Goosemoor") was originally intended as an intermediate station on the West Somerset Mineral Railway (WSMR), but neither the proposed extension to Heath Poult nor that to Joyce's Cleeve was built, leaving Gupworthy as the line's southwestern terminus. The WSMR was built primarily to carry iron ore from mines to Watchet harbour in Somerset, England. The line was unconnected to any other, though it passed under what is now the West Somerset Railway south of the village of Watchet. The station was located west of the top of the line's most striking feature - a three quarters of a mile, rope-hauled incline at a gradient of 1 in 4 (25%). From 1876 to 1883 a horse-drawn tramway brought iron ore from Kennesome Hill mine to the station, where it was transferred to WSMR wagons. The line's seven stations were designed by Rice Hopkins. Uniquely, no photograph of the station as built has been published, so whether it resembled all the others except Watchet is not known. It was built in anticipation of offering the usual goods and passenger facilities, but no regular passenger service ever ran south of Comberow. Before it was finished the building was converted into two dwellings and has now been remodelled.

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.

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.