- Bran Point
Bran Point is a small headland on the
Dorset coast in southernEngland , about half way between the small villages of Ringstead to the east andOsmington Mills to the west. There is a picturesque cliff-top path between the two villages via Bran Point.The name derives from the brown colouring of the rock forming the cliffs of the headland, caused in part by residual oil deposits. [Watson, D. F.; Hindle, A. D. and Farrimond P. (2000) "Organic geochemistry of petroleum seepages within the Jurassic Bencliff Grit, Osmington Mills, Dorset, UK" "Petroleum Geoscience" 6(4): pp. 289-297] The
geology of the area is particularly interesting. The coastline in the area is formed from rocks and shingle with exposed cliffs behind. The Middle WhiteOolite of the Osmington Oolite more visible to the west has descended to beach level here. At the middle of the cliff, there is nodular rubble consisting of calcitized spongespicule s. Higher in the cliff are reddish brown beds containing "Trigonia clavellata"fossil s [ [http://www.soton.ac.uk/~imw/osring.htm West, Ian M. (2006) "Osmington Mills to Ringstead, Dorset, UK, Corallian strata" "Internet Geology Field Guide"] ] .Notes
See also
*
Geology of Dorset
*Jurassic Coast External links
* [http://www.soton.ac.uk/~imw/osring.htm Ian West's "Geology of the Wessex Coast" Field Guide] , including photographs
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