Journal Of An Overland Expedition In Australia, By Ludwig Leichhardt




















































































































 -  For the Condamine,
although not constantly, was raised by rains, and showed the origin of
its supply, by the muddy - Page 144
Journal Of An Overland Expedition In Australia, By Ludwig Leichhardt - Page 144 of 272 - First - Home

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For The Condamine, Although Not Constantly, Was Raised By Rains, And Showed The Origin Of Its Supply, By The Muddy Nature Of Its Waters; The Dawson Commenced Running Where We Left It; And The Burdekin, With Several Of Its Tributaries, Was Running As Far As We Followed It.

The waters of the Dawson, the Burdekin, and the Lynd, were very clear, and received their constant supply from springs.

We passed a camp of natives, who vere very much alarmed at the report of a gun, which Mr. Gilbert happened to fire when very near them; this he did in his anxiety to procure a pair of Geophaps plumifera, for his collection. These pretty little pigeons had been first observed by Brown in the course of our yesterday's stage, who shot two of them, but they were too much mutilated to make good specimens. We frequently saw them afterwards, but never more than two, four, or six together, running with great rapidity and with elevated crest over the ground, and preferring the shady rocks along the sandy bed of the river. I tried several methods to render the potatoes, which we had found in the camps of the natives, eatable; but neither roasting nor boiling destroyed their sickening bitterness. At last, I pounded and washed them, and procured their starch, which was entirely tasteless, but thickened rapidly in hot water, like arrow-root; and was very agreeable to eat, wanting only the addition of sugar to make it delicious; at least so we fancied.

June 8. - We travelled about nine miles west-north-west. The country was in general open, with soft ground on the more extensive flats; although sandstone ranges approached the river in many places. Four good-sized creeks entered the river from the southward. The sandstone, or psammite, was composed of large grains of quartz mixed with clay of a whitish red or yellow colour; it frequently formed steep cliffs and craggy rugged little peaks.

The stringy-bark grew to a fine size on the hills, and would yield, together with Ironbark and the drooping tea-tree, the necessary timber for building. A new species of Melaleuca and also of Boronia were found, when entering upon the sandstone formation.

The wind for the last few days has been westerly; cumuli forming during the day, dissolved towards sunset; the days were very hot, the nights mild and dry. It was evident that we had descended considerably into the basin of the gulf.

June 9. - We travelled about ten miles north-west. Box-tree flats, of more or less extent, were intercepted by abrupt barren craggy hills composed of sandstone, which seemed to rest on layers of argillaceous rock. The latter was generally observed at the foot of the hills and in the bed of the river; it had in most places been worn by the action of water. The stringy-bark became even numerous on the flats, in consequence of the more sandy nature of the soil: but the hills were scrubby, and Mr. Gilbert reported that he had even seen the Bricklow.

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