Whitecliff Bay is a sandy bay near
Foreland which is the easternmost point of the
Isle of Wight
The Isle of Wight ( ) is a Counties of England, county in the English Channel, off the coast of Hampshire, from which it is separated by the Solent. It is the List of islands of England#Largest islands, largest and List of islands of England#Mo ...
, England, about two miles south-west of
Bembridge and just to the north of
Culver Down. The bay has a shoreline of around and has a popular sandy
shingle beach
A shingle beach (also referred to as rocky beach or pebble beach) is a beach which is armoured with pebbles or small- to medium-sized cobbles (as opposed to fine sand). Typically, the stone composition may grade from characteristic sizes rangi ...
which is over half a mile long. It is a tourist site with three holiday parks in the vicinity of the bay; it has two cafes though minimal facilities. Access is limited and only possible down two steeply sloping concrete tracks.
The site is of major geological interest, being part of the
Whitecliff Bay And Bembridge Ledges SSSI.
Geology
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
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...
beds of soft sands and clays, separated by an
unconformity
An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval o ...
from the underlying
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of ...
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 of well-exposed sands and of late
Palaeocene to late
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " ...
clays which make the site is a good spot for
fossil hunting, with an abundance of prehistoric shells, sponges and
molluscs
Mollusca is the second-largest phylum of invertebrate animals after the Arthropoda, the members of which are known as molluscs or mollusks (). Around 85,000 extant species of molluscs are recognized. The number of fossil species is esti ...
. The bay itself is shallow up to around from shore getting to deep water 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 at the south-eastern point of the bay.
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References
External links
Whitecliff Bay Holiday Park
{{Bays on the Isle of Wight
Tourist attractions on the Isle of Wight
Bays of the Isle of Wight
Geology of the Isle of Wight
Bembridge