Oakhill

Ashwick is a village in the Mendip district of Somerset, England, about three miles north of Shepton Mallet and seven miles east from Wells. It has also been a civil parish since 1826. The parish had a population of 1,352 according to the 2011 census, and apart from Ashwick village also includes Gurney Slade and Oakhill.

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.

Harridge Wood is an area of woodland in Somerset, England. From about 1300 AD part of the wood was the scene of coal mining, which continued until around 1800. The traces of mining have been well preserved, and are now a scheduled site. The woodland is now part of the Harridge Woods Nature Reserve. Large areas were planted for timber in the mid-20th century, and this continues to be harvested. The nature reserve is steadily reintroducing the original flora.

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.

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.

Christ Church is a former Church of England church in Downside, Somerset, England. Designed by John Pinch the younger, it was built in 1837–38 and closed in 1983. The church, now a private residence, is a Grade II listed building.

Windsor Hill Marsh (grid reference ST619454) is a 0.84 hectare biological Site of Special Scientific Interest, north of the town of Shepton Mallet in Somerset, and adjacent to the Windsor Hill Quarry geological Site of Special Scientific Interest. It was notified in January 1972. Windsor Hill Marsh is a marshy silted pond, with adjacent damp, slightly acidic grassland. Adjoining the marsh are a limestone bank, and a short stream which flows into a swallet.

Balch Cave (grid reference ST65734753) is a cave in Fairy Cave Quarry, near Stoke St Michael in the limestone of the Mendip Hills, in Somerset, England. The cave is part of the complex of passages feeding to St. Dunstan's Well Catchment Site of Special Scientific Interest and an abandoned Bristol Water abstraction point. It is named in honour of Herbert E. Balch who was famous for his exploration of the Caves of the Mendip Hills.The cave was broken into by quarry blasting in November 1961. Much of the cave has since been quarried away and by the end of the 1960s, major sections were destroyed.An exploration in December 1961 found a series of decorated rifts, mainly of sparkling flowstone, with a grotto fillet with pure white stalactites and pillars and a set of "organ pipes" about 10 feet (3 m) wide and 15 feet (5 m) high.A further visit in January 1962 explored the fourth chamber which is richly ornamented with white and cream flowstone, several narrow curtains, and miscellaneous white stalactites, and the fifth and sixth chambers with multiple Stalagmite formations.In the subsequent years continued blasting from the quarry breached the central chambers of the cave destroying some 425 feet (130 m) of passages, with rockfalls destroying many of the remaining formations, and rendering other sections of the cave inaccessible. Stabilisation work at the end of the quarry's life resulted in the destruction of a further 300 feet (91 m) of passage, including the original entrance series and Great Chamber.The Fairy Caves Management Committee administers the access to this cave on behalf of the quarry owners. The cave is closed from 1 October to 30 April to protect the hibernating bats.

Hillier's Cave (grid reference ST65734753) is a cave in Fairy Cave Quarry, near Stoke St Michael in the limestone of the Mendip Hills, in Somerset, England.It falls within the St. Dunstan's Well Catchment Site of Special Scientific Interest. The cave was discovered on 13 February 1954, when blasting at one of the working faces opened up a cave passage, and is now choked with sludge waste from the quarry. It was first explored by John Anthony Quinn and boys from Midsomer Norton Grammar School (now Norton Hill School) who named it in honour of Gordon Hillier who was headmaster of the school from 1926 to 1958.The Fairy Caves Management Committee administers the access to this cave on behalf of the quarry owners.

Fairy Cave Quarry (grid reference ST65734753) is between Stoke St Michael and Oakhill in the limestone of the Mendip Hills, in Somerset, England. Quarrying was first started on the site in the early 1920s. In 1963 the quarry was acquired by Hobbs (Quarries) Ltd., and production on a much larger scale began. Excavations cut back into the hillside above St Dunstan's Well Rising, a Bristol Water abstraction point (long since abandoned); various caves were intercepted. The quarry ceased production in 1977.The caves in Fairy Cave Quarry include: Balch Cave Conning Tower Cave Fairy Cave Fernhill Cave Hillier's Cave Hillwithy Cave Shatter Cave W/L Cave Withyhill CaveThe caves in the quarry were formed by water from an unknown source. Withybrook Slocker is an active swallet to the south of the quarry and although the water sinking here presently flows through the quarry caves the stream is misfit. Withybrook Slocker, however, gives access to the upstream continuation of the quarry caves and digging activities by the Cerberus Spelaeological Society will hopefully lead to the discovery of the original source of the system. The quarry has also been used extensively for climbing, with 172 named routes. Although this was previously without permission of the landowners, in July 2010 access for climbers was agreed.

Shatter Cave is a cave in Fairy Cave Quarry, near Stoke St Michael in the limestone of the Mendip Hills, in Somerset, England. It falls within the St. Dunstan's Well Catchment Site of Special Scientific Interest.The name commemorates the damage, done by blasting in the quarry, to some of the decoration within the cave.

W/L Cave is part of the Fairy Cave Quarry group of caves between Stoke St Michael and Oakhill in the limestone of the Mendip Hills, in Somerset, England. It is named after the initials of its discoverers, Bob Whitaker and Jerry Lavis, was first entered in the summer of 1967. It was the first significant cave to be discovered after the destruction of Balch Cave in the same (Fairy Cave) quarry. Although short it was extremely well decorated with calcite formations and ended in a large chamber with a magnificent side grotto dubbed Pink Pool Chamber. It is almost certainly part of the Balch Cave system and is the link between Balch Cave and the other systems in Fairy Cave Quarry namely Shatter Cave and Withyhill Cave. The link was proved by a digging project conducted by Pete Rose and Nick Chipchase of the Cerberus Spelaeological Society, the HQ of which club used to lie adjacent to the quarry in cottages owned by the quarry company. Pink Pool Chamber is linked to the first chamber in Shatter Cave by a narrow passage opened by blasting by the above named cavers.