Spinifex and Sand by David Wynford Carnegie
page 279 of 398 (70%)
page 279 of 398 (70%)
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of the desert could have had but one ending.
Our way lay over spinifex plains until just north of the hills a sand-ridge was crossed, remarkable from its regular shape and wonderfully straight course, as if it had been built to most careful measurements and alignment. The 16th of November was a red-letter day, for on it we crossed the LAST SAND-RIDGE--in lat. 19 degrees 20 minutes--leaving the desert behind us. A feeling of satisfaction filled us that we had conquered its difficulties not by chance, but by unremitting toil and patience. I am sure that each in his heart thanked his God that He had been pleased to bring us through safely. Once across the range we had seen from Mount Bannerman--a range of quartzite hills which I named Cummins Range, after the Warden at Hall's Creek--and we had reached the watershed of the tributaries of the Margaret and Fitzroy Rivers. From Cummins Range onward until we struck the Margaret, we had very rough hills and rocks to cross--this hard travelling after the yielding sand was most painful to the camels, and their feet were soon sore and cut by the sharp edges of rock. The country may be roughly described as slate bedded on edge, in such a way as to leave sharp corners and points of rock sticking up in all directions. Through the slate run veins of quartz, often rising above the surface in huge blows, hills, and even small ranges. Innumerable gullies crossed our path, and occasionally fair-sized creeks. Such a one is Christmas Creek, which, where we saw it, is made up of three creeks from fifty to eighty yards across, running almost parallel and not more than half a mile apart. These soon meet and form a fine creek which joins the Fitzroy many miles to the Westward. These creeks are fringed with gums, Bauhinia, and Leichardt trees, all affording splendid shade--and following the banks on either side is a belt of high grass and shrubs, |
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