The period from the 1st to the 5th of November was employed in taking bearings from the loftiest points of the range, both to the northward and southward of us; in examining the creek to the south-west, and preparing for a second excursion from the camp.

The rock formation of Curnapaga was of three different kinds.  A mixture of lime and clay, a tufaceous deposit, and an apparently recent deposit of soapstone, containing a variety of substances, as alumina, silica, lime, soda, magnesia, and iron.  The ranges on either side of the glen were generally varieties of gneiss and granite, in many of which feldspar predominated, coarse ferruginous sandstone, and a siliceous rock with mammillary hematite and hornblende.  These, and a great mixture of iron ores, composed the first or eastern line of Stanley’s Barrier Range.

It will be remembered that in tracing up the creek on the occasion of our first excursion from Cawndilla, that Topar had persuaded me, on gaining the head of the glen to go to the north, on the faith of a promise that he would take us to a place where there was an abundance of water, and that in requital he took us to a shallow, slimy pool, the water of which was unfit to drink.  Mr. Browne and I now went in the direction we should have gone if we had been uninfluenced by this young cub, and at less than a hundred yards came upon a pretty little clear pool of water, that had been hid from our view by a turn of the creek.  What motive Topar could have had in thus deceiving us, and punishing himself, is difficult to say.  On our further examination of the creek, however, there was no more water to be found, and from the gravelly and perfectly even nature of its bed, I should think it all runs off as fast as the channel filled.  Whilst I was thus employed, Mr. Poole and Mr. Stuart were on the ranges, and both, as well as the men generally, continued in good health; but I was exceedingly anxious about Mr. Browne, who had a low fever on him, and was just then incapable of much fatigue; nevertheless he begged so hard to be permitted to accompany me on my contemplated journey, that I was obliged to yield.

I had been satisfied from the appearance of the Williorara, that it was nothing more than a channel of communication between the lakes Cawndilla and Minandechi and the Darling, as the Rufus and Hawker respectively connect Lakes Victoria and Bonney with the Murray, and I felt assured that as soon as we should leave the former river, our difficulties as regards the supply of water for our cattle would commence, and that although we were going amongst hills of 1500 or 2000 feet elevation, we should still suffer from the want of that indispensable element.  Many of my readers, judging from their knowledge of an English climate, and living perhaps under hills of less elevation than those I have mentioned, from which a rippling stream may pass their very door, will hardly understand this; but the mountains of