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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 ]
The resistant beds of chalk and limestone form two ridges and the softer Wealden rocks between them have been eroded to form a valley. 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.
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 Lulworth Formation is a geologic formation in England.It dates from the late Tithonian to the mid Berriasian.It is a subunit of the Purbeck Group. [1] In Dorset, it consists of three members, which are in ascending order, the Mupe Member, the Ridgway Member, and the Warbarrow Tout Member.
Homocline near Lulworth Cove, England Diagram of a homocline Homocline in Aberdeenshire, Scotland. In structural geology, a homocline or homoclinal structure (from old Greek: homo = same, cline = inclination), is a geological structure in which the layers of a sequence of rock strata, either sedimentary or igneous, dip uniformly in a single direction having the same general inclination in ...
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.
[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 .
Stair Hole is a small cove located just west of Lulworth Cove in Dorset, southern England. The folded limestone strata known as the Lulworth crumple are particularly visible at Stair Hole. There are several caves visible from the seaward side of Stair Hole; Cathedral Cavern is supported by pillars of rock rising out of the water. [ 1 ]