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Lulworth Cove is a cove near the village of West Lulworth, on the Jurassic Coast in Dorset, southern England. The cove is one of the world's finest examples of such a landform , and is a World Heritage Site and tourist location with approximately 500,000 [ 1 ] visitors every year, of whom about 30 per cent visit in July and August. [ 2 ]
Some visible features along the monocline include the disharmonic folds and faults, known as the Lulworth Crumple, at Stair Hole, [2] Lulworth Cove, Arish Mell and at Peveril Point further east. These features also include the polygonal thrust ridges developed in the harder rock bands at Kimmeridge Bay and related to the growth of the monocline ...
The Fossil Forest is the remains of an ancient submerged forest from Jurassic times, located to the east of Lulworth Cove on the Isle of Purbeck in Dorset, England. [1] It lies on the Jurassic Coast, on a wide ledge in the seaside cliff. The site is within the Lulworth Ranges and thus has restricted access.
The label of Lulworth Beds was given to the strata below the Cinder Bed in 1963 by Casey, who called the remaining section the Durlston Beds. These were elevated to the status of Lulworth and Durlston Formations by Thompson in 1975, who introduced the Purbeck Group as their parent unit. Cope and colleagues considered the Purbeck as a formation ...
A visitor centre and car park occupy a hillside at Lulworth Cove, a popular attraction in the Dorset National Landscape. The coast and countryside in the National Landscape area are valued for its recreational amenity value, with the Dorset National Landscape Partnership recognising pressure from a population of 2.15 million people who live within 40 miles of the National Landscape. [1]
Mupe Bay is a bay with a shingle beach to the east of Lulworth Cove in Dorset, England, [1] and is part of the Jurassic Coast World Heritage Site. View of Mupe Rocks. The bay exposes a sequence of Cretaceous rocks from the Bindon Hill Chalk in the north through the Wealden Beds to the Purbeck Beds in the south at Mupe Rocks. [2]
[1] [2] The ridge is formed by the structure known as the Purbeck Monocline, and extends from Lulworth Cove in the west to Old Harry Rocks in the east, where it meets the sea. The hills are part of a system of chalk downlands in southern England formed from the Chalk Group which also includes Salisbury Plain and the South Downs .
Map showing two examples of how coves form. The rock types are those of Lulworth Cove. In example A, a river breaks through the resistant chalk back rock and limestone, leaving the weak clays to be rapidly eroded. In example B, the sea breaks through the limestone, perhaps by forming a cave, and then erodes the clay away.