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 : Chasm, Undercliff and New Raised Beach - Great Bindon


Chasm, Undercliff and New Raised Beach - Great Bindon

Geological section of the Chasm, Undercliff and New Raised Beach from the Eastern boundary of Great Bindon to the sea, by William Daniel Conybeare and William Dawson. The Axmouth-Lyme Regis stretch of the south coast of England comprises one of the best known areas of land slipping in Great Britain. It includes the site of the first large-scale landslide ever to have been the subject of detailed scientific description by geologists: the Great Bindon Landslide which happened on Christmas Day, 1839. Fortuitously William Buckland (1784-1856) and his scientific artist wife Mary nee Morland (1797-1857) were quickly on the spot as they had been visiting fellow geologist Wiliam Daniel Conybeare (1787-1857) in nearby Axminster. The three, along with Mary Anning (1799-1847), investigated the incident. Coloured lithograph

Picture No
14154655
Media ID
45863914
Size
5490px x 3516px (1.6MB)
Credit
© The Geological Society / Mary Evans
Source
Geological Society of London. W D Conybeare's and William Buckland's work Ten plates comprising a plan, sections, and views, representing the changes produced on the coast of East Devon, between Axmouth and Lyme Regis by the subsidence of the land and elevation of the bottom of the sea, on the 26th December, 1839, and 3rd of February, 1840', London: John Murray (1840), plate 3. - Image reference: 27-23
Date
1840

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1784-1856 1787-1857 1797-1857 1799-1847 1839 Anning Axminster Axmouth-lyme Bindon Boundary Buckland Chasm Comprises Conybeare Description Detailed Fellow Fortuitously Geological Geologist Geologists Happened Incident Includes Investigated Landslide Large-scale Morland Nearby Quickly Regis Slipping Stretch Undercliff Wiliam


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