Binegar railway station

The Anglican Church of the Holy Trinity, Binegar, Somerset, England is Norman but has been rebuilt and restored several times since. It is a Grade II* listed building.

Binegar is a small village and civil parish in Somerset, England. It is located on the A37, 4 miles (6.4 km) east of Wells, between Shepton Mallet and Chilcompton. Its population in 2011 was 313. Binegar and Gurney Slade on the opposite side of the A37 are effectively a single village and share a sign on the main road. In Gurney Slade, the quarry and houses on the north side of Tape Lane are in Binegar parish whilst the south side is in Ashwick parish. In Binegar, some houses on the south side of Station Road are in Ashwick parish and some on the north side of the village are in Emborough parish.

Gurney Slade quarry, grid reference ST626497 is a limestone quarry near Gurney Slade between Binegar and Holcombe, on the Mendip Hills, Somerset, England. Gurney Slade quarry exhibits pale to very dark grey Carboniferous Limestone overlain by red and purple-coloured Triassic breccias and marls with a small faulted block of overlying Lower Jurassic breccias forming an angular unconformity with the Carboniferous Limestone. There is abundant vertical sediment infilled fissures and joints (Neptunian Dykes). The rocks contain varying amounts of calcite mineralization, and there is common fossil material associated with the Carboniferous and Jurassic limestones. The limestone within the quarry dips to the south-east at around 30°.Work began at the quarry in the mid 18th century and grew after it was taken over by Francis Flower and Sons in 1928 producing stone for lime-burning. The quarry closed in 1947 and was reopened in 1951 by John Yeoman of Foster Yeoman. The next owner was City Sand and Gravel Co. and taken over by Morris & Perry (Gurney Slade) Ltd. who still operate the quarry. A Concrete plant was installed in 1963 and a coated macadam plant in 2001. The site is now capable of supplying up to 2 Million Tonnes Per Annum of Carboniferous Limestone aggregate. Francis Flower have a facility adjacent to the quarry which processes filler by-product from several Mendip quarries.

Emborough Quarries (grid reference ST623505) is a 1 hectare (2.5 acre) geological Site of Special Scientific Interest at Emborough in the Mendip Hills, Somerset, notified in 1971. The disused quarry has yielded a wide variety of remains of vertebrate fossils, amongst which the early reptiles are particularly well represented. Of special note is Kuehneosaurus latus which is one of the earliest-known flying vertebrates. During the Triassic period of geological time, some 230 million years ago, the limestones now exposed on Mendip formed upland areas upon which a number of large rivers rose. Solution cavities were soon created in the land surface and material from the surrounding area was swept into the newly formed cave systems. Remains of the creatures living in the upland areas during this time were swept into these deposits and have now been exhumed by recent quarrying activities. Fresh material is brought to the surface with every rock fall and Emborough Quarries are a nationally important source of fossil vertebrate remains for research and study.This former Mendip quarry site, probably owned by Emborough Stone Co., a branch of Roads Reconstruction, Ltd., where iron ore was once mined is now home to an assembly of contractor's plant (possibly of Richard Wood (Engineering) Ltd), cranes and machine tools. It is the location of Nettlebridge Viaduct, a seven-arch bridge that once carried the Somerset and Dorset Railway.The site was owned by Emborough Stone Co which was later bought by Roads Reconstruction Ltd. The rock quarried was carboniferous mountain limestone which was used for construction and railway ballast. There are 2 main quarries and several trial quarries. The site was previously used by the Emborough Brick Co for making clay bricks.

The Church of the Blessed Virgin Mary in Emborough, Somerset, England is medieval in origin but underwent extensive renovation in the 18th century. It is recorded in the National Heritage List for England as a designated Grade II* listed building. It is a redundant church in the care of the Churches Conservation Trust. It was declared redundant on 1 August 1978, and was vested in the Trust on 19 December 1979.It was originally built in the 12th century, with 14th and 18th-century alterations and some further restoration in the 19th century.The inside includes a Georgian gallery and a cast iron "Gurney Stove".The recent colour washing of the wall returned the church to its appearance before its Victorian restoration.

Maesbury Castle is an Iron Age hill fort within the parish of Croscombe on the Mendip Hills, just north of Shepton Mallet, Somerset, England. It has been listed as a Scheduled Ancient Monument.The name is derived from maes, meaning field or plain in Brythonic Welsh, and burh, meaning fort in Old English. There is also a record of the name Merksburi in 705 AD, meaning boundary fort. The area was a boundary between the Romano-British Celts and West Saxons during the period 577-652 AD, when the nearby Wansdyke fortification comprised part of the border. The enclosure has an area of 2.5 hectares (6.2 acres), and lies at a height of 292 m (950 ft), with views in many directions. This includes the Somerset Levels to Glastonbury Tor and Brent Knoll which are the closest and probably the most easily identifiable landmarks from the site. The fort has a single rampart up to 6 m high, with an outer ditch (univallate). Entrances are to the south-east and north-east (with possible outworks). The Fort and surrounding grounds are now owned by the Stevens' family who have been farming in Somerset for over 60 years.

Emborough is a village and civil parish 5 miles (8.0 km) north of Shepton Mallet, and 5 miles (8.0 km) north east of Wells, in the Mendip district of Somerset, England. It adjoins the parish of Ston Easton. It is situated on the B3139 between Radstock and Wells, just off the A37 road.

Maesbury Railway Cutting (grid reference ST606475) is a 2 hectare geological Site of Special Scientific Interest between East Horrington and Gurney Slade in Somerset, notified in 1995. It was part of the Somerset and Dorset Joint Railway. This is a Geological Conservation Review site because it exposes approximately 135 metres of strata representing the middle and upper Lower Limestone Shales and the basal Black Rock Limestone. Both formations are of early Carboniferous (Courceyan) age. It lies close to the Iron Age hill fort Maesbury Castle.

Masbury railway station was a small isolated station on the Somerset and Dorset Joint Railway's main line between Evercreech Junction and Bath. It was situated to the north of Shepton Mallet and near the summit of the line as it crossed the Mendip Hills. The station opened in 1874 and closed with the rest of the line under the Beeching Axe in March 1966. Maesbury Railway Cutting is a two hectare geological Site of Special Scientific Interest between East Horrington and Gurney Slade and a Geological Conservation Review site because it exposes approximately 135 metres of strata representing the middle and upper Lower Limestone Shales and the basal Black Rock Limestone. Both formations are of early Carboniferous (Courceyan) age. It lies close to the Iron Age hill fort Maesbury Castle. The station was never heavily used, and from 1938 it was reduced to a "halt" status. A feature of the station was a substantial stone-built stationmaster's house on the main northbound platform. The front of the house, which is still standing and in private hands, features a fanciful carving of Maesbury Castle as a medieval castle: in fact, Maesbury is an Iron Age fort nearby. There is about a half-mile of ramparts and views to Glastonbury Tor. The station is located mostly on private land but a public footpath crosses it. In May 2013 an online appeal was launched by the Somerset & Dorset Railway Heritage Trust to raise £500,000 by 30 September 2013 to purchase the station. The trust eventually raised only £80,000 by the deadline, and the site was sold to another party. The site is now in private hands so visitors are asked to respect the fact that it is a family home. Plans are in progress to restore the station to its original state, including rebuilding the signal box and renovating the platforms and waiting rooms.

Ashwick Court is Grade II* listed house on Heckley Lane northwest of Ashwick, in Mendip district, eastern Somerset, England, adjacent to the Church of St James. It is a country house, dating from the late 17th century and became a listed building on 2 June 1961. Alterations were added to the property in the 18th and mid-19th century.

Blacker's Hill is an Iron Age hill fort at Chilcompton, 4.5 kilometres (3 mi) south west of Radstock, Somerset, England. It has been designated as a Scheduled Ancient Monument.The hill fort is roughly rectangular and is a promentary type. It covers 6 hectares (15 acres) and originally had two ramparts and two ditches, but on the west and south sides it was defended by the steep drop. In some places the ramparts survive to a considerable height but on the north east side the inner rampart and ditch have been destroyed. There are three gaps but only that on the east seems to be original.In 1999 a geophysical survey was carried out suggesting that Blackers Hill originated as a univallate structure and was then later modified, forming a developed hill fort.

Oakhill is a village in the Mendip district of Somerset, England, in Ashwick parish approximately 2.5 miles (4 km) north of Shepton Mallet. It lies between the A37 and the A367 (which is part of the ancient Fosse Way). Oakhill is today is mainly a commuter village of 0.4 square miles (1.0 km2) in size, and is notable for former activities which including brewing. The village contains a Church of England primary school and a surgery, as well as a public house, the Oakhill Inn. Little London is the name given to a cluster of houses at the western end of the village. It is sometimes referred to by tradespeople etc. as a settlement in itself for the purpose of location, because of the elongated character of the village.