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Gupworthy railway station

Disused railway stations in SomersetPages with no open date in Infobox stationRailway stations in Great Britain closed in 1898Railway stations in Great Britain opened in 1861Use British English from November 2013
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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.

Excerpt from the Wikipedia article Gupworthy railway station (License: CC BY-SA 3.0, Authors, Images).

Gupworthy railway station
Stolford Hill,

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N 51.1099 ° E -3.4832 °
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Stolford Hill
TA24 7BY , Exton
England, United Kingdom
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Brendon Hills
Brendon Hills

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.

Haddon Hill
Haddon Hill

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.