Crook Peak to Shute Shelve Hill: Difference between revisions
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Most of the site is owned by the [[National Trust for Places of Historic Interest or Natural Beauty|National Trust]]. |
Most of the site is owned by the [[National Trust for Places of Historic Interest or Natural Beauty|National Trust]]. |
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A long-distance footpath, the [[Mendip Way]], follows much of the northern boundary of the site. There is a also a tunnel which was part of the [[Cheddar Valley Line]] but is now used for pedestrians and cyclists. Within the tunnel the central surface has been paved with tarmac but it is unlit except for a central guide line of small guide lamps. The north half of the tunnel is brick lined, but about midway it reverts to unlined rock for the southern half, marking a change in the underlying geology from sandstone to limestone. |
A long-distance footpath, the [[Mendip Way]], follows much of the northern boundary of the site. There is a also a {{convert|165|m}} long tunnel which was part of the [[Cheddar Valley Line]] but is now used for pedestrians and cyclists. Within the tunnel the central surface has been paved with tarmac but it is unlit except for a central guide line of small guide lamps. The north half of the tunnel is brick lined, but about midway it reverts to unlined rock for the southern half, marking a change in the underlying geology from sandstone to limestone.<ref>{{cite web|title=Exploring the Strawberry Line|url=http://www.thestrawberryline.org.uk/index.php?section=visit|publisher=The Strawberry Line|accessdate=22 April 2015}}</ref> |
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== Etymology == |
== Etymology == |
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[[Shute Shelve Cavern]] is located on Shute Shelve Hill. It is a natural cave system which was mined for its [[yellow ochre]], until the 1920s.<ref>{{cite web|url=http://www.bgs.ac.uk/mendips/localities/crookpeak.html|title=Crook Peak and Axbridge|publisher=[[British Geological Survey]]|accessdate=2009-07-07}}</ref> |
[[Shute Shelve Cavern]] is located on Shute Shelve Hill. It is a natural cave system which was mined for its [[yellow ochre]], until the 1920s.<ref>{{cite web|url=http://www.bgs.ac.uk/mendips/localities/crookpeak.html|title=Crook Peak and Axbridge|publisher=[[British Geological Survey]]|accessdate=2009-07-07}}</ref> |
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[[Black Rock Limestone]] is exposed at several sites but is commonly covered by [[Burrington Oolite]].<ref name=bgs>{{cite web|title=Crook Peak and Axbridge|url=https://www.bgs.ac.uk/mendips/localities/crookpeak.html|publisher=British Geological Survey|accessdate=22 April 2015}}</ref> |
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== Barton Camp == |
== Barton Camp == |
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Revision as of 20:21, 22 April 2015
| Site of Special Scientific Interest | |
 | |
| Location | Somerset |
|---|---|
| Grid reference | ST385555 |
| Interest | Biological and Geological |
| Area | 332.2 hectares (3.322 km2; 1.283 sq mi) |
| Notification | 1952 |
| Natural England website | |
Crook Peak to Shute Shelve Hill (grid reference ST385555) to (grid reference ST430560) is a 332.2 hectare (820.9 acre) geological and biological Site of Special Scientific Interest near the western end of the Mendip Hills, Somerset, notified in 1952.
Shute Shelve Hill, which is formed of Carboniferous Limestone laid down in the Dinantian period about 350 million years ago, rises to 233 metres (764 ft) above sea level. It is an anticline with younger limestones on the lower slopes.[1]
The site
The site extends for some 5 kilometres (3.1 mi) from west to east. Near its eastern end it is divided by a gap used by the A38 road and the disused Cheddar Valley railway line. From west to east the site includes these hills:
- Crook Peak, reaching 191 metres (627 ft), a prominent feature from the surrounding landscape. Evidence of early human occupation includes a polished flint axe. A ridge to the south east of Crook Peak, known as 'The Razor', is used by the West Mendip Soaring Association to fly model aircraft in south-westerly / southerly or north-easterly winds.[2]
- Compton Hill, above the village of Compton Bishop
- Wavering Down, reaching a height of 211 metres (692 ft)
- Cross Plain, above the village of Cross
- Shute Shelve Hill, east of the A38 road, reaching a height of 233 metres (764 ft), above the town of Axbridge and adjoining Axbridge Hill and Fry's Hill
Most of the site is owned by the National Trust.
A long-distance footpath, the Mendip Way, follows much of the northern boundary of the site. There is a also a 165 metres (541 ft) long tunnel which was part of the Cheddar Valley Line but is now used for pedestrians and cyclists. Within the tunnel the central surface has been paved with tarmac but it is unlit except for a central guide line of small guide lamps. The north half of the tunnel is brick lined, but about midway it reverts to unlined rock for the southern half, marking a change in the underlying geology from sandstone to limestone.[3]
Etymology
Crook Peak has been important as a landmark and boundary from very early times, and the origins of the name are unclear. Some believe the name 'Crook' comes from Old British 'Cruc' meaning 'peak' or 'pointed hill'.[4][5]
Somerset slang for something that is not straight is 'crook' - as in crooked
Biological
This site comprises a wide range of habitats which includes ancient and secondary semi-natural broadleaved woodland, unimproved calcareous grassland and a complex mosaic of calcareous grassland and acidic dry dwarf-shrub heath. Four of the calcareous grassland communities, two of the woodland types and the calcareous grassland/acidic dry dwarf-shrub heath mosaic all have a restricted distribution in Britain. Four nationally rare and seven notable plant species are also present. Plants of interest include the nationally rare Cheddar Pink (Dianthus gratianopolitanus), Bedstraw (Galium fleurotii), Dwarf Sedge (Carex humilis) and Dwarf Mouse-ear (Cerastium pumilum). Rose Wood and King's Wood are ancient woodland sites. The nationally rare Purple Gromwell (Lithospermum purpurocaeruleum) occurs at Rose Wood.[6]
Geological
There are cave deposits of interest at the southern end of Crook Peak. Picken's Hole is of considerable importance because of its clear, well-stratified sequence of deposits and faunas, all dating from within the Devensian. The rich Layer 3 fauna, radiocarbon dated to 34,265 (+2600/–1950) years BP, includes Spotted Hyena, Lion, Arctic fox, Mammoth, Woolly Rhinoceros, horse, reindeer, suslik and Tundra Vole. The site is a major source of information for this phase of the Middle Devensian. It is also the most carefully excavated hyena-den site and assemblage from Britain.[6]
Shute Shelve Cavern is located on Shute Shelve Hill. It is a natural cave system which was mined for its yellow ochre, until the 1920s.[7]
Black Rock Limestone is exposed at several sites but is commonly covered by Burrington Oolite.[8]
Barton Camp
Barton Camp, which is on the northern slopes of Crook Peak, is run by the Bristol Children's Help Society which was founded in 1884 to help needy children. The facilities include classrooms, a sports hall, outdoor pool, playing field and bunkhouse accommodation.[9][10]
References
- ^ Haslett, Simon K. (2010). Somerset Landscapes: Geology and landforms. Usk: Blackbarn Books. pp. 38–41. ISBN 9781456416317.
- ^ "Our location". West Mendip Soaring Association. Retrieved 21 April 2015.
- ^ "Exploring the Strawberry Line". The Strawberry Line. Retrieved 22 April 2015.
- ^ "Winscombe Parish". Retrieved 7 October 2010.
- ^ "Not a soul in the West Mendips". Times Online. London. 25 March 2006. Retrieved 18 July 2006.
- ^ a b "Crook Peak to Shute Shelve Hill" (PDF). English Nature. Retrieved 17 July 2006.
- ^ "Crook Peak and Axbridge". British Geological Survey. Retrieved 7 July 2009.
- ^ "Crook Peak and Axbridge". British Geological Survey. Retrieved 22 April 2015.
- ^ "Barton Camp". The Bristol Children's Help Society. Retrieved 21 April 2015.
- ^ Steve Eggington (August 2006). "Serious Playtime". Mendip Times. 2 (3): 10–11.