Devil's Dyke, Sussex

From Wikipedia, the free encyclopedia

LocationWest Sussex, England
Coordinates50°53′06″N 0°12′18″W / 50.885°N 0.205°W / 50.885; -0.205
Devil's Dyke
View of Devil's Dyke
Geography
LocationWest Sussex, England
Coordinates50°53′06″N 0°12′18″W / 50.885°N 0.205°W / 50.885; -0.205
Interactive map of Devil's Dyke

Devil's Dyke, also sometimes called Satan's ditch,[1] is a 100-metre (330 ft) deep V-shaped dry valley on the South Downs in Sussex in southern England, 5 miles (8.0 km) north-west of Brighton. It is managed by the National Trust, and is also part of the Beeding Hill to Newtimber Hill Site of Special Scientific Interest.[2] Devil's Dyke was a major local tourist attraction in the late 19th and early 20th centuries. It is now a popular viewpoint and site for walking, model aircraft flying and hang gliding.[3] The South Downs Way passes the site.

The Dyke is formed in rocks of the Chalk Group which originated as marine sediments during the Cretaceous period.

It is a misconception common amongst local residents of Brighton that the valley was formed by some kind of glacial action, the myth of a 'glacier' being a misunderstanding of accounts such as this one from the Encyclopaedia of Brighton by Timothy Carder (1990):

"In reality the 300-foot-deep valley was carved by tremendous amounts of water running off the Downs during the last Ice Age when large amounts of snow thawed and the frozen chalk prevented any further absorption; erosion was aided by the freeze-thaw cycle and the valley was deepened by the 'sludging' of the saturated chalk.".[4]

The Devil's Dyke V-shaped dry valley is the result of solifluction and river erosion. More than 14,000 years ago[unreliable source?], the area experienced an intensely cold climate (but not glacial conditions). Snowfields capped the South Downs. Permafrost conditions meant that the chalk was permanently frozen. In summer, the snowfields melted and saturated the top layer of soil, because the water could not permeate the frozen chalk underneath. Waterlogged material situated above the permafrost slid down the gradient, removing material by friction, exposing deeper layers of frozen chalk. When the Ice Age ended, the snowfields covering the South Downs melted, and rivers formed across Sussex. The Devil's Dyke valley was completed by one such river.[5]

Geography

The Devil's Dyke Hotel and Restaurant.

The hills surrounding the valley rise to 217 metres (712 ft) and offer views of the South Downs, The Weald, and on a clear day the Isle of Wight. It is the site of ramparts, all that remain of an Iron Age hillfort, and a pub. It is a popular local beauty spot for the Brighton and Hove area, being an easy journey of just a few miles.

History

View from Devil's Dyke

Ancient history

Before and after the Iron Age, Devil's Dyke was used as a defensive site. This was probably because of its commanding view of the surrounding terrain, and also its steep edges surrounded by large expanses of flat land.

In the Iron Age, Devil's Dyke was an important site. All the vegetation was scraped off the white chalk, leaving Devil's Dyke as an impressive monument to both attract and intimidate the populace.

Victorian times

Steep Grade Railway about 1908

In late Victorian times Devil's Dyke became a tourist attraction, complete with a fairground, two bandstands, an observatory and a camera obscura, all served by a branchline from Hove. During its heyday, Devil's Dyke was a huge attraction for the Victorians, with 30,000 people visiting on Whit Monday in 1893.

  • From 1887 to 1938 a single-track railway branch line operated from near Aldrington in Hove to The Dyke railway station, the current Dyke Farm location, to transport sightseers to the foot of the hill.
  • From 1894 to 1909 a cable car operated across the valley, covering a distance of 350 metres (380 yards), suspended 70 metres (230 ft) above the valley floor.[6]
  • From 1897 to 1909 the 3 ft (914 mm) narrow gauge funicular Steep Grade Railway rose 100 metres (330 ft) from near Poynings to the northern edge of the hillfort.

Traces remain of all three ventures, including the remains of concrete pylon supports for the cable car system.

Current use

Devil's Dyke has also become a popular site for hang gliding and (more recently) paragliding.[7]

Folklore

References

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