BASALTIC RANGE. 1300 FEET ABOVE SEA.

19th August.

At 6.45 a.m. steered south-east and soon ascended a rocky range of

altered sandstone and trap or basalt, thinly wooded with white-gum, tall

acacia, and grevillia, triodia, and treraphis superseding the grass; at

7.30 the aneroid indicated the greatest altitude (1300 feet) which we had

attained since leaving the Victoria River. From this point the view was

extensive to the north and south. Towards the interior the surface of the

tableland, not being so elevated as our position, appeared like a vast

level plain without any marked feature whatsoever. To the north the

country appeared to consist of low ridges of wooded hills gradually

decreasing in height as they receded. Southward our view was intercepted

by broken wooded hills of equal elevation with our position, while deep

ravines trending to the south intercepted our route. I therefore altered

the course to 200 degrees magnetic, and descended a rocky valley in which

was a small watercourse which enlarged into a considerable creek with

large rocky waterholes. The hills consisted of basalt and altered

sandstone, which dipped 20 degrees to 60 degrees to the north-west, and

by their outcrop formed parallel ridges which we passed with difficulty

and great risk to our horses; at 12.30 p.m. we extricated ourselves from

these ridges and entered a level valley extending thirty miles to the

north-east and south-west. Here granite rock was exposed on the bank of

the creek, which now trended across the valley to the south-east, with a

broad sandy bed from a quarter to half a mile in width, but quite dry and

overgrown with bushes; at 4.5 reached the hills which bounded the valley

to the south-east, and the creek entering a deep gorge which, by

concentrating its waters, had formed a fine pool, at which we encamped.

The country after leaving the basalt hills, where the valleys were well

grassed, was barren and useless sand, gravel, and rock.

Latitude by Vega 17 degrees 53 minutes 42 seconds.

20th August.

We left our camp at 7.0 a.m., and finding the valley of the creek

impassable, crossed the hills in an east-south-east direction, the

country consisting of steep sandstone ridges covered with triodia and a

few stunted eucalypti; at 3.0 p.m. we again attained the bank of the

creek and camped in a small patch of coarse rushes, as there was no grass

for the horses.

Latitude by Vega 17 degrees 58 minutes 7 seconds.

21st August.

Leaving this miserable spot with our starving horses, followed the creek,

which had now increased to a small river, to the east-south-east, and

after two hours' travelling reached a small patch of grass and camped at

8.20 a.m.; the bed of the river is nearly dry, only a few shallow pools

remaining in the sandy channel, which is ten to fifty yards wide, with

smaller side channels, altogether occupying a breadth of nearly 200

yards, dense clumps of melaleuca-trees growing in the intervening banks

of sand; large quantities of unio-shell, some five and six inches in

length, are found on the banks of the river near the camps of the blacks;

Bowman complains of an attack of scurvy, which causes pains in his legs

and swelling of the gums.

22nd August.

Although our yesterday's journey was only of two hours' duration, the

horses appeared very weak and fatigued when we started at 6.45 am, and it

was with great difficulty that Boco and Monkey could keep up with the

rest of the horses; we were frequently compelled to leave the bank of the

river and cross steep rocky ridges of sandstone rock; the country was

very rugged and barren, producing little besides triodia and a few

stunted gum-trees. The bed of the river increased to 400 yards in width,

consisting of sandy channels with narrow banks of sand covered with large

melaleuca-trees between them. At 1.5 p.m. camped in a small patch of dry

wiry grass; procuring water from a small pool in the bed of the river.

Latitude by Vega 17 degrees 59 minutes 2 seconds.

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