VI. BETWEEN DOVER AND SANDGATE
During the last three centuries, at all events, the coast between Sandgate and Dover has undergone considerable changes. Large quantities of stone have been removed from the Folkestone cliffs; and landslips have occurred at Shakespeare’s Cliff, between Folkestone and Sandgate, and behind East Wear Bay.[2550] It would be useless, however, for our purpose, to describe these changes in detail; for they do not affect the topographical questions that belong to the history of Caesar’s invasions of Britain. Excepting the disappearance of the little haven that once existed at Folkestone, the general character of this section of the coast was much the same in 55 B.C. as to-day. It may be, however, that the aspect of the high ground above East Wear Bay was different. Between the cliffs and the heights which rise about a quarter of a mile to the north of them there is a wild and broken plateau, called the Warren, through which the railway runs. Referring to this, William Phillips, a geologist of some repute, wrote in 1821, ‘The cliff, bounding this ruin towards the sea, is, from its position, not in situ; and it is equally clear that the enormous masses of which it is composed, have fallen forward [probably by ‘repeated falls’] from near the summit of the cliff in situ.’[2551] When these convulsions began to transform the landscape cannot, as far as I know, be ascertained.