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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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