Journals of Australian Explorations. Francis Thomas Gregory

Journals of Australian Explorations - Francis Thomas Gregory


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a way through the thicket of melaleuca on the bank of the river, returned to breakfast. At 7.50 a.m. commenced ascending, and at 8.30 reached the summit of the rocky hills, and steering about south-east through a succession of thickets, rocks, yawning chasms, sand-hills, and scrub, we attained to a fine grassy flat at 12.30 p.m. The bed of the river here quite changed its character, the sandstones giving place to granite gneiss, with dark trap dykes intersecting it in a northerly and southerly direction, the dip of the strata being to the west at a very high angle, at times almost perpendicular.

      A DEPOT CAMP. EXPLORE THE UPPER MURCHISON.

      11th October.

      As this appeared to be a good spot for the formation of a depot, while we examined the upper portion of the Murchison, I proceeded up the river in company with Mr. Burges, leaving the rest of the party to guard the camp and attend to the horses. After one hour's ride we came on our track where we crossed the river on the 25th September, the general course of the stream-bed being east-north-east, its channel averaging 100 yards in width, full of rocks, small trees, and sandbanks, with many shallow brackish pools of water, with the exception of one, which was both wide and deep, where we halted for two hours to rest the horses; few of the pools seemed likely to last through the heat of summer. At 1.0 p.m. we came on a party of natives, five of whom came up to us, following us for some distance. As they seemed to prefer mimicking our attempts to speak the York dialect to using their own, we could not obtain much information; they carried kylies and dowaks, but had left their spears and shields with the rest of their party, who did not make their appearance. At 3.0 passed several ridges of red sandstone rocks, the strata dipping to the east-north-east at an angle of from 20 to 60 degrees. The granite rock entirely disappearing, the country became quite level, and covered with one universal thicket of acacia and cypress, except the very slight depression which formed a shallow valley about three miles wide, through which the river runs in a deep channel from 80 to 100 yards wide in ordinary seasons, but when in flood must exceed 300 yards, and the rise of the water, judging from the rubbish drifted up in former years, must exceed thirty feet. The valleys did not seem to be more than 100 feet below the general surface of the country (which was quite level), filled with a dense thicket of wattles; a narrow strip of large gum-trees, growing in grassy flats close to the river, marked the course of the stream. At 5.0 we halted for the night by a small pool of fresh water in one of the back channels of the river, the pools in the main bed being all brackish.

      12th October.

      Started at 6.35 a.m., following the river, the general course being north-north-east; no change was observed in its character. At 11.20 halted to rest the horses, and again started at 1.40 p.m. At 3.40 came on a large party of natives at a fresh water pool; five followed us some miles, and were not to be satisfied until we had made an exchange of part of a handkerchief for a quantity of noolban, some dowaks, and dabbas, some of which we accepted as a token of our friendly intentions. The stream-bed turned east, and we followed it until 6.0, when we were halted for the night, having the good fortune to find a little fresh water by digging in the sand in the bed of the river, the pools being all brackish.

      RETURN TO DEPOT CAMP.

      13th October.

      At 6.15 a.m., we were again in our saddles, and continued journey up the river--the general course north-north-east. In vain we looked for some rising ground or hill from which we might obtain a view of the country, but the same sandy level, covered with dense thickets of wattles, still met the eye till 11.0, when we observed a low sandstone cliff forming the eastern side of the valley. In this direction we steered, and after pushing through thickets of wattle growing on stony ground, with small patches of salsolaceous plants, we arrived at the foot of the cliff, which was about sixty feet in height, of white sandstone, full of rounded quartz pebbles. The top was nearly on a level with the general plane of the country, which was of a most cheerless aspect. The valley of the river trended to the north-north-east for eight or ten miles, then to the east; the width appeared about five miles, and one dense thicket of wattles seemed to fill the entire space. The rest of the country was, without the slightest exception, level in the extreme, covered with one universal thicket of acacia and cypress, the latter indicating the sandy nature of the soil. As no appearance of change in the character of the country within twenty or thirty miles was visible, and we had only two days' provisions left (not having expected the stream to extend so far), and the camp at sixty miles distant, we were obliged to leave the farther examination of the river to some future explorers; but we regretted it the less as, from the nature of the gravel and sand brought down by the stream, there seemed great probability that it takes its rise in large salt marshes similar to those known to exist 100 miles east of the Irwin, if it does not actually drain them, as the general trend of the most northerly marshes seen was in the direction of the upper part of the Murchison. Under these circumstances, we returned to our bivouac of last night, reaching it at 5.40 p.m.

      14th October.

      Started at 6.25 a.m., and retracing our route down the river, came to our bivouac of the 11th at 5.5 p.m. without any incident worthy of notice, but surprising three or four natives asleep in the bed of the stream; they were of the party seen on our route up the river.

      15th October (Sunday).

      Resumed our journey; passed two parties of natives; a few of them followed us some distance, and having overcome their first surprise, commenced talking in their own language, which, as far as we could understand it, had great affinity to that spoken by the natives in the York and Toodyay districts. After a smart ride of seven hours we arrived at the encampment, found the rest of the party all well, and the horses much improved by their few days' rest.

      THE GERALDINE LEAD MINE DISCOVERED. THE HUTT RIVER.

      16th October.

      The two horses we had ridden up the river requiring a day's rest, which was also acceptable to Mr. Burges and myself, we remained at the camp and made preparations to move on to the Hutt River the next day. Mr. Walcott brought in some specimens of galena, which, on farther observation, proved to be abundant.

      17th October.

      Leaving our encampment at 9.10 a.m., we steered a southerly course, passing over a succession of low granite hills, thickly covered with acacia, to the exclusion of almost every other kind of vegetation, save a few scattered tufts of grass. At noon entered the sand-plains which occupy the high lands in this district; observed a patch of grassy land bearing south-west; proceeding in that direction, at 1.0 p.m. came on it, but found it to be a very small spot of grassy granite country, encircled by sand-plains and scrub. Continuing our course, at 2.5 struck a small stream-bed trending west-south-west; the valley in which it runs is bounded on both sides by sandy hills, covered with scrub; some patches of grass and wattles occupied the lower ground wherever the granite rock showed itself; tracing the stream-bed downwards, we found many brackish pools. At 3.45 crossed the left bank--found it running, but brackish; and at 4.20 we bivouacked at its junction with the Hutt River, which was here about ten yards wide, with narrow grassy flats on both banks. The hills are of sandstone and sand, producing little besides scrub.

      18th October.

      Started at 7.50 a.m., steering north 140 degrees east magnetic up the valley of the Hutt, which gradually widened and improved, the hills being grassy for an average distance of two miles back from the stream, of granite formation, and thinly sprinkled with wattles; behind the grassy land the country rose into sandy plains, covered with short scrub. At 9.20 crossed to the left bank; the river trended to the eastward. At 11.10 sighted King's Table Hill, bearing south magnetic. We then descended into the rich and grassy valley of the Bowes River; this we traversed till 4.0 p.m., when we bivouacked in a small stream tributary to the Bowes. As the country passed over this day had not been previously examined, we were much pleased to find it equal to the best land on the southern branch of the Bowes, visited by the Surveyor-General and myself on former occasions.

      FINE PASTORAL COUNTRY.

      19th October.

      Messrs. Burges, Bedart, and myself rode down the Bowes to examine the country, and found it generally of good grassy character, suitable for sheep; the bed of the streams being filled with broad-leaved reeds, seems to indicate an abundant supply


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