The famous geological/geographical feature Chesil Beach in Dorset, England, is a natural coastal barrier made of?
Chesil Beach the view of Chesil Beach from Abbotsbury along the coast to Portland Bill as one of the top ten in England. The origin of Chesil Beach has been argued over for some time. Originally it was believed that beach material was from the Budleigh Salterton pebble beds to the west and later from Portland to the south east. The differences between the pebbles on the beach and nearby sources is now put down to the Flandrian isostatic sea level rise, so the feature could also be considered a barrier beach or bar, that happens to connect the mainland to an
Chesil Beach Chesil Beach Chesil Beach , sometimes called Chesil Bank, in Dorset, southern England is one of three major shingle structures in Britain. Its name is derived from the Old English "ceosel" or "cisel", meaning "gravel" or "shingle". The beach is often identified as a tombolo, although research into the geomorphology of the area has revealed that it is in fact a barrier beach which has "rolled" landwards, joining the mainland with the Isle of Portland and giving the appearance of a tombolo. The shingle beach is long, wide and high. The beach and The Fleet, a shallow tidal lagoon, are