Durdle Door

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Durdle Door

Durdle Door (sometimes spelt Durdle Dor) is a natural limestone arch on the Jurassic Coast near West Lulworth in Dorset, England.

1 Geology
2 Tourism
3 Trivia
4 References
5 See also
6 External links

[edit] Geology

The arch has formed on a concordant coastline where bands of rock run parallel to the shoreline. Here the rock strata are nearly vertical, and the bands of rock are quite narrow.

Durdle Door

Originally a band of resistant Portland limestone ran along the shore, the same band which can be seen two miles down the coast forming the narrow entrance to Lulworth Cove. Behind this is a 400 ft (120 metre) band of various weaker rocks which are easily eroded, and behind this is a stronger and much thicker band of chalk, which forms the Purbeck Hills. The limestone and chalk are much closer together here than at Swanage, ten miles to the east, where the distance between them is over two miles. There are at least three reasons for this. First, the beds are highly inclined here, and more gently angled at Swanage. Secondly, some of the beds have been cut out by faulting at Durdle Door; and thirdly, the area around Durdle Door appears to have been unusually shallow, so a much thinner sequence of sediments were deposited here.

Durdle Door, Man o' War bay (opposite beach)

At Durdle bay all except a short stretch of the limestone has been completely eroded away by the sea and the remainder forms a small headland where it has protected the clay behind. At the western end this band of limestone has been eroded through, creating the natural arch.

The 400 foot isthmus which joins the limestone to the chalk is made of a 50 metre band of Portland limestone, which is less resistant than the Purbeck beds, a narrow and compressed band of Cretaceous clays—Wealden Clay, sands and chert beds—and then narrow bands of Greensand and sandstone. In Man o' War bay, the small bay immediately east of Durdle Door the Portland stone has not been entirely eroded away, and at low tide the band of Portland stone is partially revealed.

[edit] Tourism

Durdle Door is a popular tourist "honeypot," as it is a short walk from the equally popular Lulworth Cove, and lies on the South West Coast Path. Within walking distance of the car park at Lulworth are these two unique landforms, the remnants of a fossilised forest and examples of common rock types from the Jurassic and Cretaceous. The area is part of the 95-mile Jurassic Coast World Heritage Site because of its geology, and these factors make the site one of the most visited natural tourist attractions in the country, with the Lulworth estate (see: Lulworth Castle) estimating the number of hiking journeys across Hambury Tout between Lulworth and Durdle Door as being over 250,000 annually.^{[citation needed]}

[edit] Trivia

Parts of the Tears For Fears videoclip for Shout were filmed at Durdle Door.

Bruce Dickinson filmed his 'Tears of the Dragon' promo video entirely at Durdle Door.

In Nanny McPhee the children go for a picnic on the beach at Durdle Door

[edit] References

Arkell, W.J., 1978. The Geology of the Country around Weymouth, Swanage, Corfe and Lulworth, 4th pr.. London: Geological Survey of Great Britain, HMSO.
Davies, G.M., 1956. A Geological Guide to the Dorset Coast, 2nd ed.. London: Adam & Charles Black.
Perkins, J.W., 1977. Geology Explained in Dorset. London: David & Charles.
West, I.W., 2003. "Durdle Door; Geology of the Dorset Coast". Southampton University. Version H.07.09.03. http://www.soton.ac.uk/~imw/durdle.htm