tween two rocky points, that lie E.S.E., and
W.N.W. from each other, distant between three and four miles. Within
these points the Sound widens considerably, and extends in, to the
northward, four leagues at least, exclusive of the several branches
toward its bottom, the termination of which we had not an opportunity
to ascertain. But, from the circumstance of finding that the water
freshened where our boats crossed their entrance, it is probable that
they had almost reached its utmost limits. And this probability is
increased by the hills that bounded it toward the land, being covered
with thick snow, when those toward the sea, or where we lay, had not a
speck remaining on them, though, in general, they were much higher. In
the middle of the Sound are a number of islands of various sizes. The
depth of water in the middle of the Sound, and even close home to some
parts of its shore, is from forty-seven to ninety fathoms, and perhaps
more. The harbours, and anchoring-places within its circuit, are
numerous; but we had no time to survey them. The cove in which our
ships lay is on the east side of the Sound, and on the east side of
the largest of the islands. It is covered from the sea, but has little
else to recommend it, being exposed to the S.E. winds, which we found
to blow with great violence; and the devastation they make sometimes
was apparent in many places.
The land bordering upon the sea-coast is of a middling height and
level; but within the Sound, it rises almost every-where into steep
hills, which agree in their general formation, ending in round or
blunted tops, with some sharp, though not very prominent, ridges on
their sides. Some of these hills may be reckoned high, while others of
them are of a very moderate height; but even the highest are entirely
covered to their tops with the thickest woods; as well as every flat
part toward the sea. There are sometimes spots upon the sides of some
of the hills which are bare; but they are few, in comparison of
the whole, though they sufficiently point out the general rocky
disposition of these hills. Properly speaking, they have no soil upon
them, except a kind of compost, produced from rotten mosses and trees,
of the depth of two feet or more. Their foundations are, therefore, to
be considered as nothing more than stupendous rocks, of a whitish
or grey cast, where they have been exposed to the weather; but,
when broken, they appeared to be of a blueish grey colour,
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