It Is Composed Of A Pink And Whitish-Coloured Granite, With Quantities Of Calcareous Stone Near Its Base, And It Appears To Have Been Formed By The Action Of Submarine Volcanic Force.

No particular hills and no watercourses could be seen in any northerly direction.

The Gascoyne River could be traced by its valley trend for twenty-five or thirty miles eastwards, and it is most probable that it does not exist at all at fifty miles from where we crossed it. The elevation of this mountain was found to be 3400 feet above sea level, and 1800 feet above the surrounding country. The latitude of this feature is 24 degrees 44', and its longitude 118 degrees 2', it lying nearly north of Mount Churchman, and distant 330 miles from it. There were no signs of water anywhere, nor could any places to hold it be seen. It was very difficult to get a camel caravan over such a country. The night we encamped here was the coolest of the season; the thermometer on the morning of the 2nd indicated 48 degrees. On the stony hills we occasionally saw stunted specimens of the scented commercial sandal-wood and native orange-trees. Leaving the foot of this mountain with pleasure, we went away as north-easterly as we could, towards a line of hills with a gap or pass in that direction. We found a small watercourse trending easterly, and in it I discovered a pool of clear rain-water, all among stones. We encamped, although it was a terribly rough place. Arriving at, and departing from, Mount Labouchere has made some of the camels not only very tender-footed, but in consequence of the stony layers lying so up-edged, has cut some of them so badly that the caravan might be tracked by a streak of blood on the stones over which we have passed. This was not so much from the mere stones, but from the camels getting their feet wedged into clefts and dragging them forcibly out. Some were so fortunate as to escape without a scratch. We made very little distance to-day, as our camp is not more than five miles from the summit of the mountain, which bore south 61 degrees west from us. We rested at this little pond for a day, leaving it again upon the 4th.

Following the watercourse we were encamped upon, it took us through a pass, among the rough hills lying north-easterly. So soon as we cleared the pass, the creek turned northerly, and ran away over a fine piece of grassy plain, which was a kind of valley, between two lines of hills running east and west, the valley being of some width. The timber of the creek fell off here, and the watercourse seemed to exhaust itself upon the valley in a westerly direction, but split into two or three channels before ending, if, indeed, it does end here, which I doubt, as I believe this valley and creek, form the head of the Lyons River, as no doubt the channel forms again and continues its course to the west.

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