Two Expeditions into the Interior of Southern Australia — Volume I by Charles Sturt
page 27 of 247 (10%)
page 27 of 247 (10%)
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at ShoalHaven; but this river is hardly perceptible, from the summit of
the cliffs forming the sides of the Gully, which are of the boldest and most precipitous character. The ground on the summit is full of caves of great depth, but there has been a difficulty in examining them, in consequence of the violent wind that rushes up them, and extinguishes every torch. The open and grassy forests of Argyle are terminated by another of those abrupt sand-stone passes I have just described, and the traveller again falls considerably from his former level, previously to his entering on Yass Plains, to which this pass is the only inlet. From Yass Plains the view to the S. and S.W. is over a lofty and broken country: mountains with rounded summits, others with towering peaks, and others again of lengthened form but sharp spine, characterise the various rocks of which they are composed. The ranges decline rapidly from east to west, and while on the one hand the country has all the appearance of increasing height, on the other it sinks to a dead level; nor on the distant horizon to the N. W. is there a hill or an inequality to be seen. From Yass Plains to the very commencement of the level interior, every range I crossed presented a new rock-formation; serpentine quartz in huge white masses, granite, chlorite, micaceous schist, sandstone, chalcedony, quartz, and red jasper, and conglomerate rocks. It was however, out of my power, in so hurried a journey as that which I performed down the banks of the Morumbidgee River, to examine with the accuracy I could have wished, either the immediate connection between these rocks or their gradual change from the one to the other. I was content to ascertain their actual succession, and to note the general |
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