The site contains a number of unique geological features and landforms, and shows excellent examples of different landforms, including the natural arch at Durdle Door, as well as the cove and limestone folding at Lulworth. Chesil Beach has fine examples of both tombolos and storm beaches. The site has stretches of both concordant and discordant coastlines. The site is the subject of international field studies because of the quality of the geology and the example of management.
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2 Features of Interest 3 Gateway Towns 4 See Also 5 External Links |
Formation
At the start of the Jurassic period a sea level rose flooding the Triassic landscape. For most of the Jurassic period Dorset was under a tropical sea, and marine life flourished. Sediments accumulated over time, mud in deep parts, sand in shallow parts, forming shale (Kimmeridge), limestone (Lulworth to Portland) and sandstone (Studland). The bodies of dead marine animals, including dinosaurs were preserved in these sediments. A large number of particularly high quality finds were uncovered at Kimmeridge and Lyme Regis. The waters slowly fell and dinosaur footprints have been found embedded in the rocks.
In the cretaceous period the sea level rose again, this laid down more sediments which made the chalk (Old Harry Rocks, White Nothe, behind Lulworth Cove) and clays (between the Limestone and Chalk at Lulworth).
In places the earth's movement buckled the rock, forming features like the Lulworth Crumple formation. The layout of the rock, and shape of the coast making the concordant and discordant coastlines of the purbecks have led to the formation of features such as Lulworth Cove. Here the limestone has been breached and the soft clays eroded, pockets have formed under the clays where oil has accumulated as the largest onshore oil field in Britain.
Features of Interest
Gateway Towns
See Also
External Links