Mendips header
 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
Dry valleys and gorges
The Mendip plateau is incised by numerous dry valleys which deepen into spectacular gorges such as Cheddar, Ebbor, and Burrington Combe, as the steep flanks of the hills are approached. The largest of these, Cheddar Gorge, is entrenched up to 120 m deep.

The origins of these dry valleys and gorges have been debated for over a century. The earliest ideas involved earthquake rifting and similar catastrophic phenomena. The first plausible hypothesis, that the gorges were formed by cavern collapse was put forward in 1862, a myth that is still often perpetuated in many modern geological texts. This theory remained popular until 1927 when it was suggested the gorges were cut by surface rivers.

Dettifoss, Iceland
  Cheddar Gorge

Neither Cheddar or any of the other gorges and dry valleys are collapsed caverns, except possibly the Wookey Hole ravine. The size of the smallest gorge on Mendip is still far larger than even the largest Mendip caves such as GB Cave, and Lamb Leer. Many dry valleys have cut though existing cave passages. Furthermore, most stream caves on Mendip descend rapidly at first before levelling out at depth, whereas the steepest section of both Cheddar and Ebbor Gorge is near the mouth.

The Mendip dry valleys and gorges were incised over the last million years or so by meltwater rivers during the Ice Age, when the caves were blocked by ice, gravel and frozen mud. Although the area was never glaciated, the region was still deeply frozen much of the year. Torrents of summer meltwater from the snow caps poured off the hills. The material eroded during these periods was deposited as large alluvial fans (marked as 'head' on most geological maps) extending out from the gorge mouth, an excellent example occurs at Burrington Combe.

On western Mendip, many modern valleys follow earlier filled-in Triassic valleys where erosion has picked out the softer Mercia Mudstone, in preference to the harder, more resistant Carboniferous Limestone.

Apart from a few exceptions in the extreme east, all the valleys cut into the limestone are now dry. This is due to the development of underground drainage and the formation of extensive cave systems.
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