We continued a south-east route at 7.40 a.m., ascending hills of limestone and sandstone, with an upper bed of basalt, which on the higher land to the south-west was again covered by sandstone. The trap or basalt was much decomposed, and contained fragments of lower rocks. At 1.40 p.m. camped on a fine but small creek, with permanent pools of water in a rocky channel from five to thirty yards wide. The country was well grassed and openly wooded with box, sterculia, leguminous ironbark, and terminalia.
Latitude by a Trianguli Australis 16 degrees 51 minutes 55 seconds.
12th August.
At 6.50 a.m. resumed a south-east course, traversing a broken country with limestone, chert, sandstone, and trap hills, deeply cut by dry watercourses. The grass was abundant and good, though triodia appeared on the higher ridges; at 7.0 crossed a small river, with fine permanent pools of water in a rocky bed ten to thirty yards wide. The floods rise twenty feet, and extend over a breadth of 70 to 100 yards. It is the largest stream-bed crossed since leaving the river, and may possibly drain the country to a distance of sixty miles to the southward. At 1.25 camped on a small creek trending to the north-north-east, in which were pools twenty yards long and five feet deep.
Latitude by a Trianguli Australis 17 degrees 1 minute 31 seconds.
NATIVE FISHING NETS.
13th August.
Left the camp at 7.0 a.m. and continued a south-easterly course, crossing a succession of sandy valleys and broken sandstone hills; the strata horizontal, and lamina dipping to the north and east generally, but sometimes in the opposite direction; the soil poor and sandy, producing little besides white-gum and triodia. At noon ascended a high ridge, from which we saw a broad valley to the south-east, beyond which was a range of flat-topped hills terminating abruptly at the northern end, which bore east by north. Descending by a rocky ravine, at 1.30 p.m. reached a fine creek, on which we camped. This creek had deep pools of water fifty yards wide; but the steep rocky character of its banks caused the channel to appear larger than if it had been in a more level country. Under some large rocks Dean found a fishing-net made neatly of twisted bark, the mesh one and a half inch, the length perhaps thirty feet; some fishing spears showed the marks of iron tools. The rocks in this part of the country often contain angular fragments of the lower strata; thus the limestone includes fragments of chert and jasper, and the sandstone pieces of limestone, but I could not detect either granite, quartz, or slate.
Latitude by a Trianguli Australis 17 degrees 11 minutes 1 second.
14th August.