Bouv6.] 
222 
[April 17, 
rock sloping away rapidly above, it is very probable that even these 
traces, which prove a depth of 6 feet, do not give the whole of that 
of the original vessel when it was intact. Exterior to this pot 
hole, the tide sinks below the level of its bottom, but at high tide 
all is covered. 
The second kettle has its bottom three feet above that of the 
lowest one, and a perpendicular line from the centre of each shows 
the two to be three feet apart. The wall dividing them must have 
become, while yet action went on within them, very thin and prob- 
ably one broke into the other before it ceased altogether. The 
whole southern side of this second hole, which I call No. 2, is gone 
and water can only now stand in its bottom to the depth of about 
two inches. 
The concavity above this which formed the northern portion of 
the hole, exhibiting as it does a well-worn surface of 3 feet in 
width, shows it must have been as large or larger than the first. 
This concavity can be discerned to the height of 5 feet, where 
further traces are lost; but, as is the case with No. 1, the whole 
depth of the pot hole may have been much greater that what is in- 
dicated. The slope of what remains of the walls of these holes 
shows that the flow of water over the rock surfaces was from the 
northwest. That of No. 2 approximates to 30° from that direction 
towards the southeast. 
Of No. 3, so designated by me, there is but little to be said, ex- 
cept that it is small and shallow. It is 4 feet 9 inches above No. 
2 in a northwest direction, and there may be traced from it west- 
erly a narrow water channel about 6 feet in length. 
The fourth of the kettle holes which I will mention is or was the 
largest of all and hence has been called by the people near by 
the “Well.” 
Passing over the rocky elevation in a northerly direction, it may 
be found about a hundred feet distant from the others in front of a 
cliff which faces an opening in the rocks more immediately near 
the water. This pot hole, unlike those previously mentioned, is 
not found on a sloping portion of rock, but is on a flat surface di- 
rectly at the base of the cliff. Horizontally, the form of it is oval 
and its largest diameter, which is northeast and southwest in di- 
rection, is 4 feet, the narrowest 2 feet 10 inches. The depth at 
which water is now retained is about 1 foot. 
The cliff rises 9 feet high from the margin of the “Well” and 
