thumb|lulworth cove, viewed from the north lulworth cove is a cove near the village of west lulworth, on the jurassic coast world heritage site in dorset, southern england. the cove is one of the world's finest examples of such a landform, and is a tourist location with approximately 500,000 visitors a year, of whom about 30% visit in july and august.http://wayback.archive.org/web/20060221205637/http://www1.dorsetcc.gov.uk/living/facts/landusedata.nsf/6cadf4da179fc19500256663004afece/cb589f955aaeba1c80256f1e003d8c62?opendocument it is close to the rock arch of durdle door and other jurassic coast sites. lulworth cove featured on the tv programme seven natural wonders as one of the wonders of southern england. == lulworth cove == thumb|right|the formation of lulworth cove the cove has formed because there are bands of rock of alternating resistance running parallel to the shore (a concordant coastline). the seaward side the clays and sands have been eroded away. a narrow (less than 30 metre) band of portland limestone rocks forms the shoreline. behind this is a narrow (less than 50 metre) band of slightly less resistant purbeck limestone. behind this are 300â350 metres of much less resistant clays and greensands (wealden clays, gault and upper greensand). forming the back of the cove is a 250 metre wide band of chalk, which is considerably more resistant than the clays and sands, but less resistant than the limestones. the entrance to the cove is a narrow gap in the limestone bands. this was formed by a combination of erosional processes by wave action and the processes of weathering. the wide part of the cove is where the weak clays and greensands have been eroded. the back of the cove is the chalk, which the sea has been unable to erode as fast as it does not dissolve in the sea acids. the unique shape of the cove is a result of wave diffraction. the narrow entrance to the cove ensures that as waves enter they bend into an arced shape this is shown clearly on the photograph.  == stair hole == thumb|right|the formation of stair hole stair hole, less than half a mile away, is an infant cove which suggests what lulworth cove would have looked like a few hundred thousand years ago. the sea has made a gap in the portland and purbeck limestone here, as well as a small arch. the sea has made its way through to the wealdon clays and begun eroding them. the clay shows obvious signs of
Bays_of_Dorset Coves_of_England Geology_of_Dorset Jurassic_Coast Visitor_attractions_in_Dorset