Part 78

At 6.25 a.m. steered east and traversed a slightly undulating granite country, with small watercourses trending west-south-west. Ironbark and box formed an open forest, the soil poor and gritty, with a few patches of black soil, with blocks of lava on the surface. At 11.15 ascended a small hill of lava, from which the country appeared very level to the east. To the north-east large hills rose about twelve miles distant; ranges also bounded the plain to the south, and some distant summits were visible to the south-east. Continuing an east course, lava became more frequent, and at length covered the whole surface. At 2.30 p.m. came on several streams of lava, forming ridges of rugged rocks, which were crossed with difficulty. These streams of lava appeared to have run from north to south, the thickness twenty to thirty feet, and breadth very variable. The level ground was lightly timbered with ironbark and box. At 5.25 turned to the south-east, following a small gully. Passed a small native well; but very little water in it, and the rock prevented it being enlarged. At 6.15 camped near some large rocks, in which five or six gallons of rainwater had collected. Walking down the creek one and a half miles in search of water, found two small pools of rainwater; but the darkness of the night and broken nature of the ground prevented the party moving to them.

14th October.

Moved the camp to the waterholes found last night, one and a half miles down the gully. The country is here granite formation, undulating and moderately grassed, and wooded with box and ironbark. The day was cloudy, but cleared at night, and I took sights for time, latitude, and lunar distance. Chronometer 2287 would not wind up in the morning, and stopped during the day, but, having run down, wound again without difficulty.

Longitude by lunar distances 144 degrees 33 minutes 15 seconds; latitude by e Pegasi 18 degrees 41 minutes 38 seconds; variation of compass 5 degrees 50 minutes east.

15th October.

Resumed our journey at 7.0 a.m., and followed the course of the creek to the south-east. The north-east side was a plain of lava, and the south-west consisted of granite ridges with sandstone on the summits. Several small creeks joined from the south-west, and increased the principal channel considerably. At 10.0 the country was more level and openly timbered with box and bloodwood; grass was abundant and green, owing to heavy rains, which appear to have been accompanied with hail, as the west-north-west sides of the trees were much bruised and the soil indented, and a great portion of the leaves torn from the trees. At 1.15 p.m. camped on a small tributary creek. The country appears to be chiefly granite and mica schist, with thin beds or streams of lava, which have come from the ranges to the north and advanced to various distances into the more level land. The surface of the lava is more thinly wooded and better grassed than the granite; but the roughness of the surface and scarcity of water rendered it less convenient travelling. From one of the higher ridges we had a wide but imperfect view of the country. The air being hazy, only a few of the marked features of the ranges to the north were visible; to the east a high hill twenty-five miles distant rose beyond an undulating wooded country. At 6.0 a heavy thunderstorm caused the creek to run for several hours.

Latitude by Capella 18 degrees 49 minutes 13 seconds.

THE BURDEKIN RIVER. A CAMP OF LEICHHARDT'S.

16th October.

The rain having passed away, the morning was clear and cool, and at 6.35 a.m. resumed our journey, steering average south-east, crossing the creek several times, and at 11.0 reached the bank of the Burdekin River, which had a strong stream of water flowing in its channel, which is here about 100 yards wide, but full of casuarina and melaleuca trees; the banks steep and cut with deep gullies. Following the river to the south-east, at 2.0 p.m. camped in a large open grassy flat a mile from the river, obtaining water from a small pool filled by the rain last night.

Latitude by e Pegasi 18 degrees 57 minutes 48 seconds; variation of compass 5 degrees east.

17th October.

At 6.30 a.m. resumed our journey, steering east and south for two hours over level flats; then turning east crossed a steep range of sandstone hills, the strata nearly vertical; the strike north and south; thin veins of quartz intersected the rock in every direction, forming a complete network. The steepness of the country compelled us to turn north-east to the bank of the river, which we followed to the south-east; the banks were high and cut by deep gullies. At 12.30 p.m. the hills receded, and we entered some fine flats. Here I picked up a fragment of the shoulder-bone of a bullock, and observed several trees that had been cut with iron axes; and as the latitude corresponds with that of Dr. Leichhardt's camp of the 26th April, 1845, the bone doubtless belonged to the bullock he killed at this place. At 1.5 camped on the bank of the river. The Moreton-Bay ash, poplar gum, and a rough-barked gum-tree with very green leaves, were added to the ironbark, bloodwood, and other eucalypti which constituted the forest, while casuarina and Melaleuca leucodendron grow in the beds of the larger watercourses. The channel of the river is about 150 yards, with a small stream winding along the sandy bed; much of the running water is due to the late rain, but it is evident from the character of the vegetation that it continues to run throughout the dry season.

Latitude by a Cygni 19 degrees 37 seconds.

18th October.

Continued our route at 6.25 a.m., steering nearly east till 8.30, when the river turned to the north round a range of sandstone hills, crossing which, reached the river again at 10.5 flowing south, with fine openly-timbered flats on the banks; steering south till 1.0 p.m., camped on the bank of the river just below a ridge of slate rock which crossed the channel. From the hills, at 9.0, we saw a fine valley joining that of the Burdekin from the east; it was bounded by a steep range to the south, which terminated two miles from the river. South-west of our position were several flat-topped hills, which appeared to be a continuation of the range crossed yesterday. To the south only a few distant hills were visible, the view being obstructed by trees. The flats on the banks of the river are well grassed and openly timbered with ironbark, Moreton-Bay ash, bloodwood, and poplar gum; the soil varying from a soft brown loam into which our horses sank deeply, to a firm black or brown clay loam; the ranges were stony and thinly grassed; the timber box and ironbark. The geological features consist of a fine-grained sandstone interstratified with slate and coarse conglomerates. The sandstone is intersected in every direction with veins of quartz, which do not appear to enter the slate. The dip of the strata is nearly vertical, the strike north and south. The whole appear to have been much disturbed and altered; neither granite nor trap has been observed since yesterday morning. Consumed the last of the dried horse-meat, and increased the ration of flour to one pound per diem.

19th October (Sunday).

Remained at the camp to rest the party; the day was cloudy, with variable breeze from the south-east to north-east and north; no observations for latitude could be taken till early on Monday morning, and even then the altitudes were imperfect; the stream of running water in the bed of the river has increased, but is still quite clear.

Latitude by Saturn 19 degrees 7 minutes 19 seconds.

CROSS THE CLARK RIVER.

20th October.

Resumed our journey at 6.40 a.m., steering south-east through fine grassy flats till 10.0, when we crossed the Clark River, and altered the course to east over well-grassed flats, to the foot of a rocky range of sandstone hills, which we reached at noon, and ascending by a steep spur, at 2.30 p.m. attained the highest ridge; here sandstone was the prevailing rock; xanthorrhoea, silver-leafed ironbark, and triodia constituted the principal vegetation; descending gradually, at 3.30 reached a small creek with a patch of good green grass on its banks, and at 3.45 halted at some small waterholes, which appeared to be permanent; except near the creek, the country was poor and stony, with a forest of ironbark and box trees; the country between the Clark and the Burdekin appears to be of excellent quality, consisting of well-grassed flats, timbered with ironbark, Moreton-Bay ash, poplar, gum, and box trees. The Clark is about 100 yards wide, with a sandy bed crossed by ridges of slate rock; the banks are sixty to eighty feet high, and the marks of last year's flood thirty to thirty-five feet, the trees being bent and broken by the force of the current; more water appears to come down the Clark during floods, but the Burdekin has a more constant stream, the Clark containing only shallow pools of water, separated by dry sand and rock; after leaving the immediate flats of the river the country was very poor and stony; the late rains had not extended so far, and the grass had the dry and parched appearance which characterised the country on the banks of the Gilbert.

Latitude by a Pegasi 19 degrees 14 minutes 2 seconds.

FRIENDLY NATIVES.

21st October.

6.15 a.m., resumed our journey and traversed an inferior country of sandstone and porphyry; box, silver-leafed ironbark, and triodia characterized the vegetation; in crossing one of these gullies, in which were some pools of water, Bowman's horse fell over the bank into the pool, and he got some severe bruises; at 10.15 came on the river, where it ran over a ledge of rocks forming a succession of rapids, below which it spread out into a broad sheet of sand a quarter of a mile wide, and turned to the south. As Bowman had fallen some distance in the rear, I selected the first suitable spot, and at 11.0 encamped, and shortly after Mr. H. Gregory came in with Bowman to camp. On the bank of the river we saw two black gins, who climbed a tree on our approach, and in the afternoon came to the camp with an old man, and after some unintelligible conversation departed; they had neither clothes or weapons, except a throwing-stick of the same form as those used by the blacks of the southern shore of the Gulf of Carpentaria. The geological character of the country has been sandstone, much altered by contact with porphyry which has been forced through it; both dip and strike are confused, and could not be ascertained to have any general angle or direction, except in the bed of the river, where the strata dipped 10 degrees to the north, but in the hills, on the left bank below the camp, the strata was horizontal; the river is now 150 yards wide at the narrowest parts, a small stream of water, one foot deep and ten to twenty yards wide, running in a winding course through the sand, and sometimes expanding into sheets of water occupying the whole breadth of the channel.

Latitude by a Pegasi 19 degrees 16 minutes 22 seconds.

22nd October.