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ccident, or the cargo getting loose during the day's journey, frequently caused the bullocks to upset their loads and break the straps, and gave us great trouble even in catching them again:--at night, too, if we gave them the slightest chance, they would invariably stray back to the previous camp; and we had frequently to wait until noon before Charley and Brown, who generally performed the office of herdsman in turns, recovered the ramblers. The consequences were that we could proceed only very slowly, and that, for several months, we had to keep a careful watch upon them throughout the night. The horses, with some few exceptions, caused us less trouble at the commencement of our journey than afterwards, when our hobbles were worn out and lost, and, with the exception of one or two which in turns were tethered in the neighbourhood of the camp in order to prevent the others from straying, they were necessarily allowed to feed at large. It may readily be imagined that my anxiety to secure our horses was very great, because the loss of them would have put an immediate stop to my undertaking.--But I hasten to enter on the narrative of our journey. CHAPTER I LEAVE THE LAST STATION--FOSSIL REMAINS--DARLING DOWNS--ENTER THE WILDERNESS--WATERLOO PLAINS--THE CONDAMINE--HEAVY RAINS--CHARLEY'S MISCONDUCT--MURPHY AND CALEB LOST--KENT'S LAGOON--COAL--MURPHY AND CALEB FOUND AGAIN. It was at the end of September, 1844, when we completed the necessary preparations for our journey, and left the station of Messrs. Campbell and Stephens, moving slowly towards the farthest point on which the white man has established himself. We passed the stations of Messrs. Hughs and Isaacs and of Mr. Coxen, and arrived on the 30th September, at Jimba, [It is almost always written Fimba, in the Journal; but I have corrected it to Jimba.--(ED.)] where we were to bid farewell to civilization. These stations are established on creeks which come down from the western slopes of the Coast Range--here extending in a north and south direction--and meander through plains of more or less extent to join the Condamine River; which--also rising in the Coast Range, where the latter expands into the table-land of New England--sweeps round to the northward, and, flowing parallel to the Coast Range, receives the whole drainage from the country to the westward of the range. The Condamine forms, for a great distance, the separation of the sandstone co
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