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Part 67

Journals of Australian Explorations · Augustus Charles Gregory — chapter 67 of 88 · ~1,736 words · public domain

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Starting at 7.30 a.m., followed the creek to the north-east by east till 8.25, when it was joined by a small creek from the south; thus increased water was abundant in the bed of the creek, but the pools were shallow and not permanent. Grassy flats extended for a mile on each bank of the creek, beyond which the level forest of stringybark, bloodwood, and box was well grassed; the soil a good red loam. In a few spots fragments of limestone and agate were strewed over the surface, and an occasional ridge of ironstone conglomerate was crossed on which the grass was indifferent. At 12.45 p.m. camped in a wide grassy flat, where the grass, having been burnt early in the season, had sprung up again quite fresh and green.

Latitude by a2 Centauri 15 degrees 11 minutes 24 seconds; variation of compass 2 degrees 10 minutes east.

4th July.

We were again in the saddle at 7.10 a.m., and, steering 70 degrees magnetic, diverged from the creek, traversing a level grassy forest of stringybark with abundance of green grass; at 8.0 turned north-east; the forest became more open, and the stringybark was replaced by bloodwood and box; limestone rock was frequent, and rendered the surface of the country very rough; and frequent depressions of the surface appeared to result from the falling-in of the roofs of caverns beneath which were farther indicated by deep clefts and holes in the rock, into which the surface waters flow during the rains. At 11.0 a.m. turned north, and at noon again struck the creek, which gradually turned to the north-north-east; limestone formed the banks, and only one small pool was seen till 4.50 p.m., when we found a little water in the sandy bed of a tributary creek from the south-south-east, at which we encamped. On the bank of the creek we this day first observed the casuarina, which is so frequent on the banks of the creeks trending towards the Gulf of Carpentaria.

Latitude by Arcturus and a Coronae Borealis 14 degrees 54 minutes 2 seconds.

5th July.

As the course of the creek was to the north-west, and we had already been driven further north than was desirable, we left the creek and followed up the tributary to the east-south-east, leaving the camp at 7.5 a.m. The channel was soon lost on the wide grassy flats, in one of which was a fine waterhole covered with nymphae, near which a party of blacks were encamped. On our approach most of the women decamped with their bags and nets containing their valuables, while the men stood spear in hand gazing on the strange sight, as we passed them. Continuing up the creek, the course of which was only marked for some distance by the nature of the vegetation, which indicated occasional inundations, it again formed a shallow irregular channel in the centre of an open box flat, and at 1.30 p.m. camped at a small waterhole in the channel.

Latitude by meridian altitude of the sun 14 degrees 55 minutes 15 seconds.

TABLELAND.

6th July.

The small size of the creek affording little prospect of water nearer to its source, and as Mr. H. Gregory was suffering from a severe attack of fever, which rendered travelling unadvisable, I proceeded with Charles Dean to examine the country to the east-south-east. Leaving the camp at 7.0 a.m., steered 120 degrees magnetic; at eight crossed a sandstone ridge covered with acacia scrub, and again descended into the valley of the creek, passing some fine grassy plains, and at 11.0 ascended the level tableland, the edge of which was covered with acacia scrub, beyond which we passed a level flat acacia scrub and small trees, and at noon entered a stringybark forest with occasional patches of bloodwood, leguminous ironbark, and sterculia. The soil varied from a brown loam to ironstone gravel, and in a few spots ferruginous conglomerate was visible. On the loamy soil the grass was good and abundant, but the gravel was covered with spiny treraphis. This tableland was so level that no declivity could be detected during the continuance of our day's journey, which lasted till 5.30, when we bivouacked without water; by taking the precaution of letting the horses feed on the outward track, and secreting ourselves after dark in the high grass, we passed the night without the necessity of keeping watch after midnight.

7th July.

Our horses having strayed back on the track, we carried our saddles and tracked them about two miles, and then mounting our horses steered north for some miles; but all was level forest without any sign of the existence of water, except a few cockatoos. I then turned to the south-west; crossing the outward track, and at length came on a shallow watercourse trending west, a ridge of rocks having confined the channel to a narrow space; three small waterholes were discovered in which a little water remained; below this the creek turned south-south-east, and I again turned towards the camp; but night overtaking us in the stringybark forest, we passed to the south of the camp without observing its position.

8th July.

Having ascertained that we had passed the position of the camp, turned to the north-east and reached the camp at 11.20. Mr. H. Gregory was somewhat recovered, but very weak from a violent attack of fever. During my absence a small party of blacks had visited the camp and had bivouacked a short distance up the creek.

9th July.

Moved the camp to the waterholes twelve miles south-east, and in the afternoon rode down the creek with Mr. Elsey; the creek turned to the south-south-east for a mile and a half, and was lost on a level flat, from which a channel trended to the west, which was again lost in a level flat extending to the west several miles. Heavy showers at night.

CIRCUMCISION PRACTISED.

10th July.

Accompanied by Mr. Elsey, I proceeded to reconnoitre the country to the south-east, and at 7.45 a.m. steered 130 degrees, gradually ascending the tableland, and which was openly wooded with bloodwood, box, and white-gum; acacia and sterculia occasionally appearing. The soil was brown sandy loam with a few ridges of sandstone rock of white colour; grass had been abundant, but was now burnt off. The small white-ant nests from two to five feet high were very numerous; at 12.40 p.m. a slight depression in the country was observed, and limestone appeared, and deep hollows were frequent. One of these hollows which I examined was thirty yards in diameter and fifteen feet deep; in the centre was a deep cleft of fifteen feet more, which extended to the east and west under the surface with a width of three feet; at 3.0 struck a small creek trending east-north-east with a few small pools of water in the channel; in following down the creek in search of a sufficient supply of water for the horses, we passed some blacks sitting at a fire near the creek; at 3.30 came to a pool sufficient for the supply of the whole party, below which the channel was dry; returning to the pool we met the blacks following our tracks, but, observing us, they ran away, and on being followed hid themselves; having unsaddled, we commenced our dinner and soon saw the blacks watching us from their hiding places, and after some time spent in making signs, they were induced to approach, the oldest of the party feigning to weep bitterly till they got close to us, when we commenced an attempt at conversation, and they appeared to recognise some few words of the language of the Victoria River. Their spears were formed of reeds with large heads of white sandstone, and also with three wooden points for fishing. They were circumcised and had their front teeth remaining; at 5.0 steered to the west-north-west for one hour, and bivouacked to secure ourselves from an attack during the night.

11th July.

At 6.30 a.m., resumed our route towards the camp, and reached it about 1.0 p.m., without observing anything of farther remark.

Latitude by a2 Centauri 15 degrees 2 minutes 49 seconds.

ABSENCE OF WATERCOURSES.

12th July.

The grass near the camp having been burnt off, the horses had scattered very much, and could not be collected and saddled before 10.0 a.m., when we followed our track of yesterday and reached the pool of water at sunset. The country was so level, although we were crossing the watershed between the north-west coast and the Gulf of Carpentaria, that the aneroid only varied from 29.55 to 29.62, and even of this change the greater part was caused by alteration of the temperature. The geological character of this portion of the country differs slightly from that of the Victoria River. The upper stratum is a bed of ironstone conglomerate about twenty feet thick, this rests on sandstone, the upper part of which is highly ferruginous, then passes away into a variegated sandstone imperfectly stratified, changing into a hard siliceous sandstone which is white and breaks with a conchoidal fracture; this rests on a hard cherty sandstone similar to that of the Victoria River. In this rock many depressions occur, which is apparently caused by the roofs of caverns falling in and there are usually deep fissures in the rock at the bottom of these hollows, in which all the water that drains into them is absorbed; in some places the sandstone resting on the limestone has sunk many feet below the general level, with areas varying from one to ten acres, sometimes sloping towards a centre ten to thirty feet below the plain, and in other spots with abrupt rocky banks five to eight feet high and a perfectly level bottom. The level character of the country is unfavourable for investigations of this nature, and the thickness of the several strata not easily determined; but I think that the collective thickness of the several strata above the limestone does not exceed 100 feet. The porous nature of the lower rocks preclude the existence of permanent surface water by draining the whole of the upper part of the tableland, while it forms strong springs in the lower ground towards the banks of the Roper River, where the limestone is exposed on the surface.

Latitude by a Coronae Borealis 15 degrees 14 minutes 31 seconds.

WHITE MAN'S CAMP.

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