and the rapidity of the flood tide was
observed to increase with the increasing contiguity of the shores. When
the sloop was on the point of entering the harbour, which appeared to be
fairly open before her, the water shoaled suddenly, and she struck the
ground and lay fast; but fortunately the strong flood in a few minutes
dragged her over into deep water, and shot her into the entrance with
uncommon velocity.
Having advanced within the entrance, the harbour began to expand itself
in a kind of large basin. Its shores were broken into points and
projections, between some of which the great strength of the flood tide
led them to expect it would branch off into arms. The land lying
immediately upon its borders was low, but not flat; well wooded; and
those points near which the sloop passed were clothed with a very unusual
degree of verdure. The sun being down, the vessel was anchored for the
night, and the next day they proceeded with their researches.
They were employed during sixteen days in the examination of this place;
and the result of the observations which were made by Mr. Bass in
different parts of it, and the neighbouring country, are thrown by that
gentleman into one general account.
This harbour, or inlet, which was named by the governor Port Dalrymple,
in compliment to Alexander Dalrymple, esq takes its course from the SE
between two chains of rounded mountains, stretching inland from the sea
with an almost imperceptible increase of elevation; and, after gradually
approximating each other, seemed to unite, at the distance of between
thirty and forty miles, in a body of rugged mountains more lofty than
themselves. These two chains in their relative positions formed an acute
angle, being at their greatest distance asunder, as measured along the
sea coast, only sixteen miles.
Being limited in point of time (twelve weeks having been deemed by the
governor sufficient for the execution of this service), the apprehension
of losing a wind favourable for the prosecution of the principal object
of the voyage, that of sailing through the strait, deterred them from
attempting to reach the head of the river; but it was hardly to be
doubted, that its principal source proceeded from some part near the
point of union of the two chains of mountains. Allowing this supposition,
a great part of its stream must be perfectly fresh; for at the place
where they ended their examination, which was not more than half the
whole
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