Our
coastal landscapes have been formed by water. Sedimentary rocks
were deposited by water and have been acted upon by rain, river
and waves.
About 85 million
years ago a huge shallow sea covered the Transmanche region
-
Sussex, Kent, Pas de Calais and Normandy. Chalk up to 350 metres
deep was formed from the remains of foraminifera, microscopic
marine animals which swam in the then tropical sea.
Movements in the
earths crust caused an uplifting of the chalk in the Miocene
period
(5-23 million years ago). The subsequent erosion of the folds
forms the basis of todays land forms. The shape of the
coastline has been created by repeated rising and dipping of
the land relative to the sea.
Only 10,000 years
ago, when Northern Europe went through a very cold climatic
period, England was connected to the mainland. But the climate
changed and sea levels rose as ice sheets melted. About 5,000
years ago the sea broke through the chalk hills joining the
channel to the North Sea and created an island.
Web Links: www.brighton.ac.uk/environment/ROCC