Overview maps
 Locality areas
  Cheddar Gorge
 Burrington Combe
 Shipham & Rowberrow
 Crook Peak & Axbridge
 Banwell to Churchill
 Harptree & Smitham Hill
 Draycott & Westbury-sub
 Wookey Hole & Ebbor
 Great Elm & Vallis Vale
 Mells & the Wadbury Valley
 The Vobster area
 The Whatley area
 Torr Works & Asham Wood
 Beacon Hill
 Stoke St Michael & Oakhill
 Holwell & Nunney
 Shepton Mallet & Maesbury
 Gurney Slade & Emborough
 The Nettlebridge valley
 Rocks of Mendips
 Geological timescale
 Ancient environments
 Geological structure
 Minerals and mines
  Minerals and mines
 Industrial archaeology
  Stone as a resource
 Employment & the economy
 Quarrying & geodiversity
 Quarrying & the environment
 History of quarrying
 Caves and karst
 How caves form
 Dry valleys and gorges
 Dolines and sinkholes
 Mendip caves
 Going caving
  Flora and fauna
 Typical Mendip habitats
 Special Mendip habitats
 Horseshoe bats
 Appendix of names
 Biodiversity of western
 Biodiversity of eastern
 External links
 Detailed site information
  Coal mining
  Mendip quarry companies
  East Mendip quarries
 Biodiversity of eastern
  West Mendip quarries
 Biodiversity of western
 Site map
The Nettlebridge valley

The Somerset Coalfield stretches from the Mendips north to Pensford and Timsbury, and is centered around the town of Radstock. It was in this coalfield that William 'Strata' Smith, the so-called 'father of English geology', first put together his ideas on stratigraphy. The southernmost part of the coalfield extends south to the Mendip Hills. Here the Mells River has incised the Nettlebridge valley, cutting through a cap of Dolomitic Conglomerate to expose the Upper Carboniferous Coal Measures beneath. The area contains a wealth of interesting geology, industrial archaeology and wildlife, as well as several nature reserves.

  Aerial view of the Nettlebridge valley (click to enlarge view).

Coal mining
Coal was probably worked in Roman times but mining began in earnest in the 1600s. The early pits exploited surface outcrops, but by the 1790s, shafts up to 150 m deep were being sunk. However, the rocks are highly contorted and are often vertical or even overturned, which has made coal mining in the area very difficult. Because of the thin near-vertical seams, the miners employed techniques more akin to Cornish tin mines than traditional methods used elsewhere. However, the narrow contorted seams made production expensive and competition from more economical coalfields led to the closure of the last remaining pit in 1973.
  Old bridge on the former Dorset and Somerset Canal

The remains of several pits can be seen in the valley including Moorewood Colliery near Upper Benter, Strap Pit (renamed Mendip Colliery in 1953 by National Coal Board) and New Rock Colliery. Abundant evidence of pre-18th century mining can be seen in Harridge Wood, Edford Wood and around Benter. In these areas the coal seams outcrop at the surface and the remains of old bell pits, spoil heaps, adits and shafts create a very hummocky topography.

Map of the old coal mines. Click to enlarge.
Map of the old coal mines. (Click to enlarge).

There were plans to connect the mines in this area to a proposed Bristol–Poole canal. In the end, only about 13 km of canal was cut, the remains of which can be seen around Edford and Coleford where the canal crossed a valley by a two-arched viaduct known locally as the Hucky Duck. A footpath now runs along its course.

More information about coal mining in Somerset is available from Radstock Museum.

The pit head at the Mendip colliery, 22 August 1962, click to view larger.
The pit head at the Mendip colliery, 22 August 1962. (Click to enlarge).

Flora and fauna

The Nettlebridge contains several nature reserves including Harridge Wood and Edford Wood. Both are thought to be very old, but have been locally coppiced or felled and replanted with conifers. Where the woods retain their semi-natural character, there is a very rich woodland flora. The distribution of species closely reflects underlying variation in geology, soil wetness and pH. The area is particularly good for bats, including rare greater and lesser horseshoe bats, which roost in caves and buildings nearby. Daubenton's bats forage along rivers and streams, particularly in the western arm of Edford Wood.

Bluebells in Harridge Wood


Toothwort (Lathraea squamaria) a perennial parasitic plant which feeds on plant roots.
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