Writhlington

Writhlington is a suburb of Radstock and 6 miles (10 km) north-west of Frome in the Bath and North East Somerset district of Somerset, England.

Writhlington
Residential housing along a road at the top of a hill with other buildings visible in the distance.
Houses at the top of the hill in Writhlington
Writhlington is located in Somerset
Writhlington
Writhlington
Location within Somerset
OS grid referenceST699545
Civil parish
Unitary authority
Ceremonial county
Region
CountryEngland
Sovereign stateUnited Kingdom
Post townRADSTOCK
Postcode districtBA3
Dialling code01761
PoliceAvon and Somerset
FireAvon
AmbulanceSouth Western
UK Parliament

History

The ancient parish of Writhlington was part of the Kilmersdon Hundred.[1]

Church

The parish church was dedicated to St Mary Magdalene. It has been designated by English Heritage as a Grade II listed building.[2] The church has since been converted to a private residence, whose owners have included the actor Dai Bradley.[3] The old rectory which accompanies it dates from the 18th century.[4] There is also a Methodist church dating from the early 20th century.

Coal mining

Coal pits within the village were part of the Somerset coalfield and the site is now Writhlington Site of Special Scientific Interest, which includes 3,000 tons of Upper Carboniferous spoil from which more than 1,400 insect fossil specimens have been recovered, including Phalangiotarbida,[5] and Graeophonus.[6] and the world's earliest known Damselfly,[7] It is a Geological Conservation — Protected Site.[8]

In 1896[9] they were owned by Writhlington, Huish and Foxcote Colliery Co., and by 1908[10] this had been changed to Writhlington Collieries Co. Ltd. The Upper and Lower Writhlington, Huish & Foxcote were all merged into one colliery. Most of the output went to Portishead power station.

The village was on a branch of the proposed route of the Somerset Coal Canal, however this was converted into a tramway in 1815.[11]

Geology

The base of the Kilmersdon Valley is of alluvium deposits. Above this on both sides of all of the valleys is a band of shales and clays from the Penarth Group. These rocks are from the Triassic period. The majority of the remaining upland in this area is Lias Limestone (white and blue) while the very highest part above 130 m, south of Haydon, is a small outcrop of Inferior Oolitic Limestone. All these limestones are from the Jurassic period. The steepest slopes of both the Kilmersdon and Snail's Bottom Valleys have frequently slipped. Below all of the area is the coal-bearing Carboniferous strata. Haydon is an outlier of Radstock and was built to house the miners for the local pit. The disused railway line and inclined railway at Haydon form important elements within the Kilmersdon valley east of Haydon. The modern landscape has a less maintained and 'rougher' character and texture than neighbouring agricultural areas. This is caused in the main by the remnants of the coal industry and its infrastructure and changes in agricultural management. The disturbance caused by coal mining and the railways and the subsequent ending of mining and disuse of the railways has created valuable habitats of nature conservation interest.[12]

Sport

Andy Robinson taught Mathematics, Physical Education and Rugby at Writhlington School.

The village cricket team plays in the North Somerset Cricket League.

References
  1. "Somerset Hundreds". GENUKI. Retrieved 16 October 2011.
  2. "Church of St Mary Magdalen". historicengland.org.uk. Retrieved 13 January 2008.
  3. "Top 15 unusual buildings for sale". The Daily Telegraph. Archived from the original on 2 January 2013.
  4. "The Old Rectory". historicengland.org.uk. Retrieved 13 January 2008.
  5. Pollitt, J.R.; Braddy, Simon J. & Dunlop, Jason A. (2004): The phylogenetic position of the extinct arachnid order Phalangiotarbida Haase, 1890, with reference to the fauna from the Writhlington Geological Nature Reserve (Somerset, UK)
  6. Dunlop, J.A. (1994). "An Upper Carboniferous amblypygid from the Writhlington Geological Nature Reserve". Proceedings of the Geologists' Association. 105 (4): 245–250. doi:10.1016/S0016-7878(08)80177-0.
  7. Duncan, I. J.; Titchener, F.; Briggs, D. E. G. (2003). "Decay and Disarticulation of the Cockroach: Implications for Preservation of the Blattoids of Writhlington (Upper Carboniferous), UK". PALAIOS. 18 (3): 256. Bibcode:2003Palai..18..256D. doi:10.1669/0883-1351(2003)018<0256:dadotc>2.0.co;2.
  8. "Writhlington SSSI, Somerset". English Nature. Archived from the original on 29 September 2007. Retrieved 14 November 2006.
  9. "Peak District Mines Historical Society Ltd". Archived from the original on 15 July 2011. Retrieved 10 October 2010.
  10. "List of Mines in Great Britain and the Isle of Man, 1908". Coal Mining Resource Centre. Retrieved 12 November 2006.
  11. Priestley, Joseph (1831). Historical Account of the Navigable Rivers, Canals, and Railways, of Great Britain. p. 580. Retrieved 9 December 2007.
  12. "Rural Landscapes — Area 15 Norton Radstock Southern Farmlands" (PDF). Bath and North East Somerset Council. Retrieved 6 April 2018.

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