On Mr. Roper's return, he informed me that he had met with a creek at the other side of the hills to the east of us; that the hills were covered with dense scrub, teeming with wallabis; and that the creek went to the north-east, several other creeks joining it; that, lower down, it was lined with Casuarinas, and that about seven miles from the hills, he found fine water-holes.
CHAPTER V
DIFFERENCE OF SOIL AS TO MOISTURE
PHILLIPS'S MOUNTAIN
ALLOWANCE OF FLOUR REDUCED AGAIN
HUGHS'S CREEK
TOMBSTONE CREEK
CHARLEY AND BROWN BECOME UNRULY
THE ISAACS
NATIVE WOMEN
COXEN'S PEAK AND RANGE
GEOLOGICAL CHARACTER
CHARLEY REBELS AGAIN AND LEAVES
BROWN FOLLOWS HIM
BOTH RETURN PENITENT
VARIATIONS OF THE WEATHER
SKULL OF NATIVE
FRIENDLY NATIVES VISIT THE CAMP.
Feb. 2.--Being much recovered, I took both Blackfellows with me, and again passed the defile east of Roper's and Scott's Peaks, and followed the watercourse rising from it to the northward. About two or three miles lower down, we found water in deep rocky basins in the bed of the creek. The rock was sandstone, fissured from south-west to north-east.
In passing the foot of the peaks, we found a species of Grewia (Dwarf Roorajong) covered with ripe fruit; the fruit is dry, but the stringy tissue which covers the seed, contains a slightly sweet and acidulous substance of a very agreeable taste. The fig-tree with a rough leaf, had plenty of fruit, but not yet ripe. Erythrina was both in blossom and in seed.
Sending Brown back to conduct our party to the water-holes we had found, and leaving the creek, which turned to the eastward, I continued my ride to the northward. I passed some gentle well-grassed slopes of narrow-leaved Ironbark and spotted gum; and also several basaltic ridges, which head out into small plains gently sloping to the east and north-east. They are formed of a rich black soil, and generally a shallow creek meanders through them: sandstone ridges formed their boundary lower down, where, at their foot, water-holes generally existed, either with a constant supply of water, or readily filled by thunder-showers. The basaltic ridges, as well as the plains, were covered with a fine crop of dry grass; but the sandstone ridges were frequently scrubby. The difference between the sandstone country and the basaltic plains and ridges, is very striking in respect to the quantity of water they contain: in the latter, rain is immediately absorbed by the cracked porous soil, which requires an immense quantity of moisture before it allows any drainage; whereas the sandstone forms steeper slopes, and does not absorb the rain so quickly, so that the water runs down the slopes, and collects in holes at the foot of the hills parallel to the creeks. Scrubs are frequent round the low rises of sandstone; and, where the country is level, and the soil loamy, the hollows are often filled with water by the thunder-storms. The moist character of this description of country is probably the cause of the vegetation being more dense than it is in the rich black soil of the plains; in which latter, the seeds of the grasses and herbs lie dormant, until the first rain falls, when they instantly germinate and cover the plain with their rapid and luxuriant growth, as if by enchantment; but which, from its nature, is incapable of maintaining the growth of scrubs and trees.
Feb. 3.--The dew was heavy through the night; and, in the morning, loose rainy clouds gathered from the east and north-east, which, however, disappeared about eleven o'clock. Charley went back to the camp, to bring it on, and I continued to reconnoitre to the north-west. After passing a sandstone ridge, I came to a creek, which went to the north-west, and which was supplied with water by the late thunder-showers. It was bounded on both sides by sandstone ridges, whose summits were covered with scrub and Acacia thickets; and by grassy slopes and flats bearing narrow-leaved Ironbark and Bastard-box. This would be a most beautiful country, if it contained a constant supply of water.
I observed on the ridges an Acacia, a small tree, from thirty to forty feet high, and from six to nine inches in diameter, and easily distinguished by its peculiar rough frizzled bark, similar to that of the Casuarina found at the ranges of the Robinson. It has a dark sweet-scented heartwood, like that of the Bricklow and the Myal and other Acacias, which I had previously met with. The creek turned to the north and north-east, into a plain, and joined a larger creek which came in from the right at about south-west. Near their junction, a very conspicuous peak was observed, with several small water-holes with water at its foot. I then returned to the spot to which Charley had been ordered to conduct the camp; but, as the party had not arrived, I feared that some accident might have happened, and therefore rode towards the water-holes from which Brown had gone back to the camp. I found the detention caused by the absence of the horses, which had strayed to the other side of the range.
Feb. 6.--Charley rode my horse after the missing ones, and returned with them about one o'clock to the camp; and then we proceeded about six miles due north, in the direction of a fine mountain of imposing character-- which I called "Phillips's Mountain," after one of my companions--and encamped in sight of Calvert's and Scott's Peaks, the former of which bore S. 22 degrees W., and the latter S. 7 degrees E. Our latitude was 22 degrees 43 minutes.