Whitecliff Bay
The site is of major geological interest, being part of the Whitecliff Bay And Bembridge Ledges SSSI.
Geology
![](http://upload.wikimedia.org/wikipedia/commons/thumb/2/23/Whitecliff_Bay%2C_IW%2C_UK.jpg/220px-Whitecliff_Bay%2C_IW%2C_UK.jpg)
Whitecliff Bay has nearly identical geology to the lesser known Alum Bay, being a coastal section of the same strata which run east–west across the island. It displays a classic sequence of fossil-bearing Eocene beds of soft sands and clays, separated by an unconformity from the underlying Cretaceous Chalk Formation forming the headland of Culver Down to its south. Due to geological folding of the Alpine orogeny, the strata in the main section of the Bay are vertical, with younger rocks to the north. In the bay, there are around 500 metres (1,600 ft) of well-exposed sands and of late Palaeocene to late Eocene clays which make the site is a good spot for fossil hunting, with an abundance of prehistoric shells, sponges and molluscs. The bay itself is shallow up to around 350 metres (1,150 ft) from shore getting to deep water 1⁄2 nautical mile (0.6 mi; 0.9 km) out.
History
Whitecliff Bay was one of the landing points for the French invasion of the Isle of Wight (1545) where they planned to go on to attack Sandown. The bay gets its name from the chalky cliff on the headland, Culver Down, which rises over 340 feet (104 m) at the south-eastern point of the bay.
References
- ^ Google (5 September 2018). "Sandown Bay" (Map). Google Maps. Google. Retrieved 5 September 2018.
- ^ West, Ian M. 2007. [1], Geology of the Wessex Coast of England. School of Ocean and Earth Science, National Oceanography Centre, Southampton, Southampton University. Internet site. Version: 25 July 2007, retrieved 3 August 2008
- ^ "Whitecliff Bay". UK Fossil Collecting. 8 February 2008.
- ^ "Whitecliff Bay". eoceanic.com. Retrieved 6 September 2018.
- ^ "Pilot the Isle of Wight: Puckaster Cove to Bembridge". Yachting Monthly. 20 June 2012.