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ters which I had written. The boat was not ready at the time appointed, and Mr. Scott returned to the tents. In the evening, however, he again went to the settlement, and about ten, P.M., he, and the man who was to manage the boat, went on board to sail for Adelaide. I had been taken very ill during the day, and was unable to accompany him to the place of embarkation. The following is a copy of my despatch to the Governor, and to the Chairman of the Northern Expedition Committee, embodying my reasons for going to the westward. "Port Lincoln, October, 1840. "Sir,--Having fallen back upon Port Lincoln for supplies, an opportunity has occurred to me of writing a brief and hurried report of our proceedings. I have, therefore, the honour to acquaint you, for the information of His Excellency, the Governor, and the colonists interested in the Northern Expedition, with the result of my examination of the country north of Spencer's Gulf, and of the further steps I contemplate taking to endeavour to carry out the wishes of the Committee, and accomplish the object for which the expedition was fitted out. "Upon leaving our depot, near Mount Arden, the low, arid, and sandy nature of the country between the hills and Lake Torrens, compelled us to follow close under the continuation of Flinders range. Here our progress was necessarily very slow, from the rugged nature of the country, the scarcity of water, and the great difficulty both of finding and obtaining access to it. As we advanced, the hills inclined considerably to the eastward, gradually becoming less elevated, until, in latitude 29 degrees 20 minutes S., they ceased altogether, and we found ourselves in a very low and level country, consisting of large stony plains, varied occasionally by sand; and the whole having evidently been subject to recent and extensive inundation. These plains are destitute of water, grass, and timber, and have only a few salsolaceous plants growing upon them; whilst their surface, whether stony or sandy, is quite smooth and even, as if washed so by the action of the water. Throughout this level tract of country were interspersed, in various directions, many small flat-topped elevations, varying in height from 50 to 300 feet, and almost invariably exhibiting precipitous banks. These elevations are composed almost wholly of a chalky substance, coated over on the upper surface by stones, or a sandy soil, and present the appearance of having fo
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