Abstract
We do not propose to enter into the questions of the source whence the pebbles of the Chesil Beach are derived, nor of the way in which they are heaped up; these and other like matters having been almost exhaustively treated by Mr. J. Coode, to whose paper we refer the reader for a detailed account of the bank. The subject with which we propose to deal is simply the cause of the formation pf a long shingle-bank, separated from the mainland by a strip of water. This has not been noticed at length by any writer, as far as we know, though three theories of the origin of the bank have been brought forward.
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