65 deg. 22', Cape Virgin-Mary
must lie in: 67 deg. 52', which is the longitude I have assigned to it, and
which, I have reason to think, cannot be far from the truth.
The strait of Magalhaens, and the east coast of Patagonia, are laid down
from the observations made by the late English and French navigators.
The position of the west coast of America, from Cape Victory northward,
I have taken from the discoveries of _Sarmiento_, a Spanish navigator,
communicated to me by Mr Stuart, F.R.S.
Falkland Islands are copied from a sketch taken from Captain M'Bride,
who circumnavigated them some years ago in his majesty's ship Jason; and
their distance from the main is agreeable to the run of the Dolphin,
under the command of Commodore Byron, from Cape Virgin Mary to Port
Egmont, and from Port Egmont to Port Desire, both of which runs were
made in a few days; consequently no material errors could happen.
The S.W. coast of Terra del Fuego, with respect to inlets, islands, &c.
may be compared to the coast of Norway; for I doubt if there be an
extent of three leagues where there is not an inlet or harbour which
will receive and shelter the largest shipping. The worst is, that till
these inlets are better known, one has, as it were, to fish for
anchorage. There are several lurking rocks on the coast, but happily
none of them lie far from land, the approach to which may be known by
sounding, supposing the weather so obscure that you cannot see it. For
to judge of the whole by the parts we have sounded, it is more than
probable that there are soundings all along the coast, and for several
leagues out to sea. Upon the whole, this is by no means the dangerous
coast it has been represented.
Staten Land lies near E. by N. and W. by S., and is ten leagues long in
that direction, and no where above three or four leagues broad. The
coast is rocky, much indented, and seemed to form several bays or
inlets. It shews a surface of craggy hills which spire up to a vast
height, especially near the west end. Except the craggy summits of the
hills, the greatest part was covered with trees and shrubs, or some sort
of herbage, and there was little or no snow on it. The currents between
Cape Deseada and Cape Horn set from west to east, that is, in the same
direction as the coast; but they are by no means considerable. To the
east of the cape their strength is much increased, and their direction
is N.E. towards Staten Land. They are rapid in Str
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