The Hills Forming These Watersheds Are Almost Uniformly Composed Of Granite, And Generally Lie In Almost Parallel Lines, Nearly East And West.

They are mostly flat-topped, and at various points present straight, rounded, precipitous, and corrugated fronts, to the astonished eyes that first behold them.

A few small water-channels rise among them, and these, joining others of a similar kind, gather strength and volume sufficient to form the channels of larger watercourses, which eventually fall into some other, dignified by the name of a river, and eventually discharge themselves into the sea. Between the almost parallel lines of hills are hollows or narrow valleys, which are usually as rough and stony as the tops of the hills themselves; and being mostly filled with scrubs and thickets, it is as dreadful a region for the traveller to gaze upon as can well be imagined; it is impossible to describe it. There is little or no permanent water in the whole region; a shower occasionally falls here and there, and makes a small flood in one or other of the numerous channels; but this seems to be all that the natives of this part of the country have to depend upon. If there were any large waters, we must come upon them by signs, or instinct, if not by chance. The element of chance is not so great here as in hidden and shrouded scrubs, for here we can ascend the highest ground, and any leading feature must instantly be discovered. The leading features here are not the high, but the low grounds, not the hills, but the valleys, as in the lowest ground the largest watercourses must be found. Hence we follow our present creek, as it must run into a larger one. I know the Ashburton is before us, and not far off now; and as it is the largest river? in Western Australia, it must occupy the largest and lowest valley. The number of inhabitants of this region seems very limited; we have met none, an occasional smoke in the distance being the only indication of their existence. In the hot months of the year this region must be vile in the extreme, and I consider myself most fortunate in having the cool season before me to traverse it in. It is stony, sterile, and hideous, and totally unsuited for the occupation or habitation of the white man.

CHAPTER 5.3. FROM 7TH MAY TO 10TH JUNE, 1876.

Depart for higher ground. Rainfalls. Ophthalmia. Romantic glen. Glen Ross. Camels on the down grade. Larger creek. The Ashburton. No natives. Excellent bushes for camels. A strange spot. Junction of several creeks. Large snake. Grand Junction Depot. A northerly journey. Milk thistle. Confined glen. Pool of water. Blind with ophthalmia. Leading the blind. Dome-like masses. Mount Robinson and The Governor. Ophthalmia range. Rocky spring. Native fig-trees. A glen full of water. Camels nearly drowned. Scarcity of living things. And of water. Continued plague of flies. A pretty view. Tributaries join. Nicholls's Fish ponds. Characteristics of watering places. Red hill. Another spring. Unvarying scene. Frost, thermometer 28 degrees. A bluff hill. Gibson's Desert again. Remarks upon the Ashburton. The desert's edge. Barren and wretched region. Low ridges and spinifex. Deep native well. Thermometer 18 degrees. Salt bush and Acacia flats. A rocky cleft. Sandhills in sight. Enter the desert. The solitary caravan. Severe ridges of sand. Camels poisoned in the night. In doubt, and resolved. Water by digging. More camels attacked. A horrible and poisonous region. Variable weather. Thick ice. A deadly Upas-tree.

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