Spinifex and Sand<br />A Narrative of Five Years' Pioneering and Exploration in Western Ausralia by David Wynford Carnegie (best motivational books of all time TXT) 📗
- Author: David Wynford Carnegie
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There are three lagoons (or deep clay-pans) connected by a shallow, sandy channel. They are entirely surrounded by sandhills, excepting at one spot, where a narrow creek breaks through the sand-ridge. Of the three the largest and most South-Westerly one is nearly circular, and has a diameter of 600 yards with a depth varying from 1 ft. 6 in. to 4 ft. 6 in. It is capable of holding considerably more water than we saw in it. The bottom is of rock, a sort of cement in which ironstone is visible in the middle, and of clay near the edges. From the N.W. a narrow channel enters, traceable for a distance of two miles to a cane-grass swamp; into this, small watercourses, and the tail end of a larger creek lead.
Following up this flat, it will be found to develop into a defined channel running through a grassy flat timbered with bloodwoods (a kind of eucalyptus). This creek rises in the sandstone tablelands to the N. of Mount Allott, and in it at its head, is situated Alexander Spring (Forrest. 1874).
Illustration 17: Alexander SpringRound the foot of these hills, extending to the lagoon, is a fine little plain of grass, saltbush, and numerous low shrubs, all excellent feed for stock. Mounts Allott and Worsnop are certainly remarkable hills, perhaps 200 feet above the surrounding country, quite flat on the top, which is covered with scrub. From the latter the lagoon is visible, one mile distant on bearing 150°. Our camp at the lagoon was in lat. 26° 10´, long. 124° 48´. This reckoning placed Alexander Spring in a position agreeing very closely with that given it by Forrest, which was very gratifying to me. This water was marked by Forrest as “permanent.” He says in his journal:—
July 13th…Fine water at this place. I have no doubt water is always here. I named it Alexander Spring after my brother, who discovered it. Abundance of water also in rock-holes.This was in 1874. Since that date this spot has been revisited, first and not long after Forrest, by W. W. Mills, who was commissioned to bring over a mob of camels from South Australia. He followed Forrest's track from water to water, at first with no difficulty; depending on Alexander Spring, he made a longish dry stage, reached the spring only to find it dry, and had a bad time in consequence. The second party to follow Forrest's route was that of Carr-Boyd in 1896, whom Breaden accompanied, and who was prospecting for an Adelaide syndicate. They passed by this spot, but having plenty of water, as it was raining at the time, did not visit the spring. From Mount Worsnop, Woodhouse, one of the party, sighted the lagoon; but neither he nor any of the party had troubled to see whether it was salt or fresh, or of what extent it was. I have named it after Woodhouse, who first saw it. Breaden had told me of the fact of his having seen it, but I had supposed that, as rain was falling, Woodhouse was only looking on a shallow pool that could by no possibility hold water for long.
Shortly after Carr-Boyd, there followed Hubbe's party. He was sent out by the South Australian Government to follow Forrest's route, to ascertain its suitability or otherwise for a stock route. Hubbe found the spring dry, or practically so, and was much disappointed. He did not happen to find the lagoon, and had a long stage before he found water. His party arrived at Menzies shortly before we started. I was unable to get any information from him beyond the opinion that the country was worthless and a stock route impracticable. I put more faith, however, in Breaden, whose life has been spent amongst stock and travelling cattle. When with Carr-Boyd he came to the conclusion that as far as the Warburton Range cattle could be taken without much trouble; and indeed in 1873, so I have read, Gosse drove some bullocks as far as that point, which was the furthest west he penetrated when attempting to cross the Colony.
From the Warburton Range to Lake Wells the awkward part came in, but now this lagoon and the Empress Spring go far to bridge it over. I have no doubt that a fortnight's work at both these places would be sufficient to make splendid wells, supposing that the lagoon was found dry and the spring too hard to get at. At the expenditure of no great amount I feel confident that a serviceable stock route could be formed, easily negotiated in the winter months and kept open by wells during the rest of the year. The country through which the route would pass is excellent as far as the border. From there it would be necessary to hit off the small oases which are met with near Mount Squires, Warburton Ranges, Blyth Creek, and Alexander Spring. From this point the route could be taken to Empress Spring, thence to Lake Wells (or direct to Lake Wells) and the Bonython Creek, and from there to Lake Darlot there would be no difficulty. The only really bad bit of the route would be between Woodhouse Lagoon and Lake Wells, and this is no great distance. Whether the scheme would be worth the expenditure necessary to equip a really serviceable well-sinking party I am unable to judge; but it seems to me that it would be a tremendous advantage to Central Australian cattle owners to be able to drive their bullocks direct to the West Australian goldfields, even though they could only do so in the winter, at which season alone it is probable that the feed would be sufficiently good. The fact that Forrest with his horses traversed this route is evidence enough that at some seasons certain surface waters exist at no great distances apart—in some cases large supplies. For cattle to follow the route that we had come so far would be manifestly absurd, and these remarks, especially where the country between Woodhouse Lagoon and Lake Wells, and between that lake and Lake Darlot is discussed, are made with the further knowledge of these regions that our return journey gave us.
Illustration 18: Woodhouse LagoonIt seems a remarkable fact that while a spring should be found dry, not five miles from it a fresh-water lagoon with millions of gallons in it should exist. In the first place Alexander Spring is no spring; Sir John Forrest told me himself that at the time of naming it he was very doubtful. Hubbe dug it out to bedrock and proved it to be merely a local soakage in the gravelly bed of a narrow gully. Now a heavy downpour sufficient to run the creek and fill the lagoon must certainly first fill the spring and neighbouring pools. But the water in the spring would soon evaporate, whilst the depth and area of the lagoon would save its contents from diminishing from this cause, for a much longer period. So that after all it is easily understandable that we should find the lagoon full and the so-called spring dry.
Near the foot of Mount Allott we found Hubbe's camp, and in it several straps and hobble-chains; two tin-lined packing cases had been left behind, and from them we took the lids, not quite knowing to what use we could put them, but yet feeling they might be serviceable; and indeed they were.
On the summit of the hill Forrest had raised a cairn of stones; this had been pulled down by the natives and subsequently replaced by Hubbe. The blacks had again started to take it to pieces; I rebuilt what they had removed and placed on the cairn a board on which I wrote directions to the lagoon, in case any other traveller should pass.
By the side of the little creek to the North-West of the hill a bloodwood tree has been marked on one side with the number of Mills's camp, and on the other with a record of the objects of Hubbe's expedition, S.R. standing presumably for “Stock Route.”
The flat on which these trees are growing is, in my opinion, a very likely spot for finding water by sinking.
CHAPTER VII The Great Undulating Desert Of GravelOn August 22nd we left this kindly little oasis and directed our course to the North. We were now nearly in the centre of the Colony, and had made enough easting, a general northerly course being necessary to take us through the heart of the great unknown. It was my intention to steer due North for as long a period as possible, only deviating from it when forced by the exigencies of water-hunting, and when it became necessary, to bear somewhat to the eastward so as to hit off the vicinity of Hall's Creek. Unless absolutely forced to do so, I did not propose to make any deviation to the Westward—for from our small caravan it was incumbent upon us to waste no time, unless we could do so in country where game was procurable. So far, although our actual line of march had been through unmapped country, we had traversed a region already crossed by another party, whose route ran parallel to ours and some forty miles to the north. Not that that was of the least benefit to us any more than if we had been at sea; but it gave us the feeling that we were not in an absolutely terra incognita. From the lagoon, however, our route lay through country untrodden by any white man, with the exception of Ernest Giles, whose track we should cross at right angles, about one hundred miles North of Alexander Spring. But unless we sighted the Alfred and Marie Range, named by him, we should have no guide, excepting our position on the chart, to show us where we crossed the path of a caravan which marched through the wilderness twenty years before.
To give a description of the country that we now encountered, from day to day, would be so deadly monotonous that the kindest reader would hardly forgive me; and even if it could serve any useful purpose I should hesitate to recount the daily scene of solitude. A general account of this country, followed by any incidents or personal adventures worthy of notice, will suffice to give an idea of this dreary region.
From lat. 26°S. to lat. 22° 40´ there stretches a vast desert of rolling sand, not formed in ridges like those already described, nor heaped up with the regularity of those met with further north. “Downs” I think is the only term that describes properly the configuration of the country. “The Great Undulating Desert of Gravel” would meet all requirements should it be thought worthy of a name. In this cheerless and waterless region we marched from August 22nd until September 17th seeing no lakes, nor creeks, nor mountains; no hills even prominent enough to deserve a name, excepting on three occasions. Day after day over open, treeless expanses covered only by the never-ending spinifex and strewn everywhere with pebbles and stones of ferruginous sandstone, as if some mighty giant had sown the ground with seed in the hope of raising a rich crop of hills. The spinifex here cannot grow its coarse, tall blades of grass—the top growth is absent and only round stools of spines remain; well was it named Porcupine Grass!
Occasional clumps of mulga break the even line of the horizon, and, in the valleys, thickets or belts of bloodwood are seen. In these hollows one may hope to find feed for the camels, for here may grow a few quondongs, acacia, and fern-tree shrubs, and in rare cases some herbage. The beefwood tree, the leaves of which camels,
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