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 SUBMERGENCES IN HISTORIC TIMES 25 All of these subaqueous mountain-top lands or hidden elevated plateaus are conspicuously nearer the ocean surface than the real depths of the sea so much nearer that they inevitably raise the suspicion of having been above that surface within the knowledge and memory of man. It is notorious that coasts rise and fall all over the world in what may be called the normal non-spasmodic action of the strata, and sometimes the movement in one direc- tion upward or downward seems to have persisted through many centuries. If we assume that Gettysburg Bank has been continuously descending at the not extravagant rate of two feet in a century, then it was a considerable island above water about the period dealt with by the priests of Sais. Apparently the rising of Labrador and Newfoundland since the last recession and dis- persion of the great ice sheet has been even more. Here the ele- ments of exact comparison in time and conditions are lacking; nevertheless, the reported uplift of more than 500 feet in one quarter and nearly 700 in another is impressive as showing what the old earth may do in steady endeavor. It must be borne in mind, too, that a sudden acceleration of the descent of Gettys- burg Bank and its consorts may well have occurred at any stage in so feverishly seismic an area. All considered, it seems far from impossible that some of these banks may have been visible and even habitable at some time when men had attained a moderate degree of civilization. But they would not be of any vast extent. FACTS AND LEGENDS As TO SUBMERGENCES IN HISTORIC TIMES Westropp has made an interesting and important disclosure of the legends of submerged lands with villages, churches, etc., all around the coasts of Ireland. In some instances they are believed to be magically visible again above the surface in certain condi- tions; in others the spires and walls of a fine city may at times, it is thought, be still seen through clear water. Nearly, if not quite, every one of them coincides with a shoal or bank of no great depth, the upjutting teeth of rocks, or a barren fragmentary islet vestiges perhaps of something more conspicuous, extended, and alluring. Westropp says: "When we examine the sea bed, we see