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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 ]
Durdle Door, a natural arch near Lulworth Cove. Once your image is uploaded to Commons or Wikipedia, you will probably want to use it in an article. Simply click Edit on the article you want to include the image in, then add the following where you want the image to appear: [[File:Image name.jpg|thumb|Caption for the image]] For example:
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 ...
The Lulworth Estate is a country estate located in central south Dorset, England. Its most notable landscape feature is a five-mile stretch of coastline on the Jurassic Coast , a World Heritage Site , including Durdle Door and Lulworth Cove .
Freshwater Bay, Isle of Wight is an example of an area of concordant coastline - the town of Freshwater is situated on a cove which formed in the hard chalk coastline.. In coastal geography, a concordant, longitudinal, or Pacific type coastline occurs where beds, or layers, of differing rock types are folded into ridges that run parallel to the coast. [1]
Between Lulworth Cove and Kimmeridge the path passes through the Lulworth Ranges, which are not always open to the public. [69] [70] When the ranges are in use a 12-mile (19 km) road detour is needed. The coast path then reaches St Alban's Head, just to the south of the village of Worth Matravers.
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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.