Church of the Blessed Virgin Mary, Emborough

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.

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.

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.

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 railway station was a station on the Somerset and Dorset Joint Railway in the county of Somerset in England. Opened on 20 July 1874, the station consisted of two platforms, with a building on the down platform. There was a substantial goods yard with two sheds and sidings, controlled from a 24 lever signal box. Being the first station north of the line's summit at Masbury Binegar was also where locomotives used as banking engines on north-bound trains would drop off and cross the line ready to return south. The station closed to goods in 1963: passenger services were withdrawn when the SDJR closed on 7 March 1966.

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.

The Anglican Church of St Mary the Virgin in Ston Easton, Somerset, England, is a Grade II* listed building dating from the 11th century, with a 15th-century embattled 3-stage west tower.The most striking interior feature is the Norman chancel arch, with semi-circular head and colonettes. The pews, choir stalls, altar rails, pulpit, font and screen are all 19th century. There are several 18th and 19th century wall monuments particularly to the Hippisley Coxe family of Ston Easton Park, who have their own chapel at the east end of the north aisle.The chancel was rebuilt in 1707 and the south aisle around 1800.The church underwent significant rebuilding in the 19th century, by Arthur Blomfield, which included dismantling most of the building including the Norman arch, marking each stone and then rebuilding them in the same position.The parish is part of the benefice of Chewton Mendip and the archdeanery of Wells.

Ston Easton is a linear village and civil parish in the English county of Somerset. It is 14 miles (23 km) southwest of Bath and 7 miles (11 km) north of Shepton Mallet. It forms part of the Mendip district and lies along the A37 road 11 miles (18 km) south of the cities of Bristol and Bath and to the west of the town of Midsomer Norton. The parish includes the hamlet of Clapton.

Ston Easton Park is an English country house built in the 18th century. It lies near the village of Ston Easton, Somerset. It is a Grade I listed building and the grounds are listed Grade II on the Register of Historic Parks and Gardens.The current house was built around 1750 to 1760 on the site of a Tudor building. The architect may have been Thomas Paty. It was occupied by the descendants of the commissioning owner, John Hippisley-Coxe, until 1956. Since then owners including William Rees-Mogg and Peter Smedley have been involved in restoring the house, which is now in use as a private house for events. The two-storey house has a symmetrical facade with projecting wings either side of the central doorway with a Tuscan portico. The interior of the stone house is decorated with extensive plaster mouldings to ceilings and fireplaces. The grounds and gardens were laid out by Humphry Repton, but have since been reduced in size.

Chewton Mendip is a village and civil parish in the Mendip district of Somerset, England. It is situated 4 miles (6 km) north of Wells, 16 miles (26 km) south of Bath and Bristol on the A39 very close to the A37. The village is in a valley on the Mendip Hills and is the source of the River Chew. The parish includes the hamlets of Bathway and Green Ore.

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.

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.