that I had passed in these mountains, there was, probably, a sufficiency, but there was no land fit for the purposes of farming.  In other situations, on the contrary, there might be found abundance of good soil, considered unavailable for any purpose except grazing, because it had no frontage (as it is termed) on a river or chain of ponds.  Selections have been frequently made of farms, which have thus excluded extensive tracts behind them from the water, and these remaining consequently unoccupied, have continued accessible only to the sheep or cattle of the possessor of the water frontage.

In these valleys of the Upper Wollombi, we find little breadth of alluvial soil, but a never-failing supply of water has already attracted settlers to its banks—­and those smallfarmers who live on a field or two of maize and potatoes—­and who are the only beginning of an agricultural population, yet apparent, in New South Wales—­show a disposition to nestle in any available corner there.  But on the lower portion of the Wollombi, where the valley widens, and water becomes less abundant, the soil being sandy, I found it impossible to locate some veterans on small farms, which I had marked out for them, because it was known that in dry seasons, although each farm had frontage on the Wollombi Brook, very few ponds remained in that part of its channel.

Join the party.

November 27.

Early this morning, I had a visit from Mr. Finch, who was very anxious that I should attach him to the exploring party.  As I foresaw, that some delay might occur in procuring provisions, without his assistance, in this district, I accepted his services, and gave him his instructions, conditionally.  I met Mr. White at the junction of the Ellalong, and we proceeded together, down the valley of the Wollombi.

The sandstone terminates in cliffs on the right bank of this stream near the projected village of Broke (named by me in honour of that meritorious officer, Sir Charles Broke Vere, Bart.) but the left bank is overlooked by other rocky extremities falling from the ranges on the west, until it reaches the main stream.  The most conspicuous of these headlands, as they appear from that of Mattawee behind the village of Broke, is called Wambo.  This consists of a dark mottled trap with crystals of felspar.  But the most remarkable feature in this extensive valley, is the termination thereupon of the sandstone formation which renders barren so large a proportion of the surface of New South Wales.  This, in many parts, resembles what was formerly called the iron-sand of England, where it occurs both as a fresh and saltwater formation.  The mountains northward of this valley of the Hunter consist chiefly of trap-rock, the lower country being open, and lightly wooded.  The river, although occasionally stagnant, contains a permanent supply of water, and consequently the whole of the land on its banks, is favourable for the location of settlers, and accordingly has been all taken up.  The country, and especially the hills beyond the left bank, affords excellent pasturage for sheep, as many large and thriving establishments testify.  At one of this description, belonging to Mr. Blaxland, and which is situated on the bank of the Lower Wollombi, Mr. White and I arrived towards evening, and passed the night.