134 A, EF. Verrill—The Bermuda Islands; Geology. 
white, staring gaps in the dark rocks as a reminder, for many a day 
to come, of the visitation.” 
A week after this storm the great landslide at Deep Bay occurred, 
hastened, no doubt, by the effects of the great sea-waves of the 
storm. (See below.) 
During such storms, and even in those of much less violence, the 
fine calcareous mud of the shallower bays and sounds is so thoroughly 
stirred up that the water becomes milky white everywhere, and when 
this sediment settles it must make layers of notable thickness. 
Landslides. 
Owing to the undercutting of the cliffs, great masses weighing 
many thousands of tons sometimes suddenly slide off imto the sea, 
causing a great commotion. One of the latest of these landslides 
Figure 33b.—Cavernous and undercut cliff at Clarence Cove. 
happened at Deep Bay, near Hamilton, Oct. 6, 1903, a week after 
the hurricane of Sept. 28. 
An account of it was published in the Royal Gazette for Oct. 10, 
1903, as follows :-— 
“ At ‘Deep Bay,’ near Admiralty House, on Monday, about mid- 
night, (just one week after the storm) a large portion of the cliff, 
