Church of St Mary, Brompton Regis

Brompton Regis (formerly known as Kingsbrompton) is a village and civil parish in the Somerset West and Taunton district of Somerset, England about 5 miles (8.0 km) north-east of Dulverton. It is situated on the River Pulham in the Brendon Hills within the Exmoor National Park, close to Wimbleball Lake, a water supply reservoir constructed in the 1970s and completed in 1979. According to the 2011 census the village had a population of 449. The parish boundary is marked by the River Exe which is crossed by the medieval Chilly Bridge and Hele Bridge. The Haddeo is crossed by Bury Bridge.The parish includes the village of Withiel Florey, where the Church of St Mary Magdalene has 12th-century origins and has been designated as a Grade II* listed building, and the hamlets of Bury, Gupworthy and Hartford.

Haddon Hill is a prominent east–west aligned ridge in west Somerset, England, close to Hartford within the civil parish of Brompton Regis. It lies on the south-eastern fringe of Exmoor National Park though is separated from the Exmoor massif itself by the valleys of the rivers Haddeo and Exe The highest point of the ridge at OS grid reference SS 962286 is crowned by a trig point at 1,164 feet (355 m) above sea level. Much of the upper part of the hill is mapped as open access under the Countryside and Rights of Way Act 2000 and hence available for public access on foot. A couple of public footpaths traverse the hill north–south whilst numerous tracks run along its length. The larger part of the hill is within the national park, the boundary of which runs along the B3190 road which runs diagonally across the eastern end of the ridge en route from Watchet to Bampton. Vehicular access is available off this road. The hill affords views across Wimbleball Reservoir which occupies the Haddeo valley immediately to its north. Along with its eastern neighbour, Heydon Hill, Haddon Hill is largely formed from the Pickwell Down Sandstones, a thick sequence of Devonian age sedimentary rocks. The stone has been quarried in the past.A tree ring, surrounded by a bank and ditch, on the hill was previously thought to be a Bronze Age tumulus although this is no longer the case. There is a Bronze Age cairn which is 9.3 metres (31 ft) in diameter. Several Roman coins have been found at Hadborough at the western end of Haddon Hill.During World War II a military camp was built on the hill with several buildings to accommodate soldiers from the United States Army during the buildup to the Normandy landings in 1944.

Bury Bridge at Bury in the parish of Brompton Regis within the English county of Somerset is a medieval packhorse bridge. It has been scheduled as an ancient monument and Grade II* listed building.The stone bridge carries a track over the River Haddeo. It consists of four spans, two of which are 7 feet (2.1 m), one 8 feet (2.4 m) and the other 10 feet (3.0 m). Two of the arches are pointed and the other two semi-circular. It has a total span of 48 feet (15 m) and is 6 feet 6 inches (1.98 m) wide.

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 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.

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.

Bury Castle near Brompton Regis in the English county of Somerset was an Iron Age univallate hillfort which was reused with the creation of a motte after the Norman Conquest. It has been designated as a scheduled monument.

Barlynch Priory (also known as St Nicholas's Priory and sometimes spelled Barlich Priory) in Brompton Regis, Somerset, England was an Augustinian priory founded by William de Say between 1154 and 1189 and dissolved in 1537.In the late 15th century the prior was John Chester, one of the sons of Alice Chestre who made donations to the church. In 1524 the priory was at its largest with nine canons.The only visible remains are some fragments of walling attached to Barlynch farmhouse, which have been designated as a Scheduled Ancient Monument (Somerset County No 182). It has been added to the Heritage at Risk Register because of the risk of collapse.Some of the stained glass from a Jesse window at the Priory is now in the St Peter's Church in Huish Champflower.

The River Haddeo on Exmoor in Somerset, England flows from the Wimbleball Lake to the River Exe. The valley of the river consists of three tributary valleys extending down from the surrounding farmland to merge with the River Haddeo in the south. The tributary valleys include the River Pulham, which passes the village of Brompton Regis and continues to Hartford where it joins the Haddeo.In 2001 - 2002 South West Water commissioned a detailed assessment of fish population, physical habitat, flow and water quality data within the River Haddeo, since it has been subject to regulated releases from Wimbleball Reservoir, to identify potential bottlenecks restricting the development of juvenile salmon populations.

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.

Dulverton was a rural district in Somerset, England, from 1894 to 1974. It was created in 1894 under the Local Government Act 1894. In 1974 it was abolished under the Local Government Act 1972 and responsibilities transferred to West Somerset. The parishes that were part of the district included: Brompton Regis, Brushford, Dulverton, Exford, Exmoor, Exton, Huish Champflower, Skilgate, Upton, Winsford and Withypool and Hawkridge.

St George's Church, Morebath is a Grade II* listed parish church in the Church of England Diocese of Exeter in Morebath, Devon. It is part of the Hukeley Mission group of parishes, which also includes St Michael & All Angels Bampton, St Peter's in Clayhanger, St Petrock's in Petton and All Saint's in Huntsham.