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good forest land; and on the 10th we had the satisfaction to fall in with the first stream running northerly. This renewed our hopes of soon falling in with the Macquarie, and we continued upon the same course, occasionally inclining to the eastward, until the 19th passing through a fine luxuriant country, well watered, crossing in that space of time _nine_ streams, having a northerly course through rich vallies; the country in every direction being moderately high and open, and generally as fine as can be imagined. No doubt remained upon our minds that those streams fell into the Macquarie, and to view it before it received such an accession, was our first wish. On the 19th we were gratified by falling in with a river running through a most beautiful country, and which I would have been well contented to have believed the river we were in search of. Accident led us down this stream about a mile, when we were surprised by its junction with a river coming from the south, of such width and magnitude, as to dispel all doubts as to this last being the river we had so long anxiously looked for. Short as our resources were, we could not resist the temptation this beautiful country offered us, to remain two days on the junction of the river, for the purpose of examining the vicinity to as great an extent as possible. Our examination increased the satisfaction we had previously felt: as far as the eye could reach in every direction, a rich and picturesque country extended, abounding in limestone, slate, good timber, and every other requisite that could render an _uncultivated_ country desirable. The soil cannot be excelled, whilst a noble river of _the first magnitude_ affords the means of conveying its productions from one part to the other. Where I quitted it its course was northerly, and we were then north of the parallel of Port Stevens, being in latitude 32 degrees 45' South, and 148 degrees 58' East longitude. It appeared to me that the Macquarie had taken a north north-west course from Bathurst, and that it must have received immense accessions of water in its course from that place. We viewed it at a period best calculated to form an accurate judgment of its importance, when it was neither swelled by floods beyond its natural and usual height, nor contracted within its limits by summer droughts: of its magnitude when it should have received the streams we had crossed, independent of any it may receive from th
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