The Bracklesham Group consists of four geological formations: Wittering, Earnley,
Marsh Farm and Selsey. They outcrop on the coastline of Bracklesham Bay where exposures
are dependent on low tides and removal of sand cover. The sediments are mostly sands
and silts and are rapidly eroded when exposed to tidal action.
The deposits reflect deposition in shallow marine or coastal marsh environments.
The better known sediments are the marine sequences of the Earnley and Marsh Farm
Formations, which are rich in fossils.
The shell beds just south-east of Bracklesham are a spectacular site when fully exposed.
Many people find it difficult to believe that these are shells really 45 million
At Selsey, the marine sediments (illustrated) are now rarely exposed following construction
of the Bunn Leisure beach and rock groynes. One bed forms the off-shore rock reefs
known as The Hounds and The Mixon, the latter about 1km south of the tip of Selsey
Bill. The Mixon was formerly worked for a building stone and the older parts of Selsey
are mostly built of it. The stone was also used by the Romans, who favoured Mixon
for well lining. It can also be see at Fishbourne Roman Palace
The Selsey coastline was once the most rapidly eroding coastline in Britain. Even
today, the sea defences cannot protect against the most severe storms. As a consequence
of this, the Environment Agency have created a managed coastal retreat scheme, the
largest in the UK.
The scheme was completed in 2013 with the breaching of the former shingle bank at
the Broadrife Sluice. The sea is now rapidly eroding the coastline and exposing historic
alluvial muds and soils (see photo). The new wetlands are now managed by the RSPB.