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we traversed. Among these there are some varieties of granite, rock-crystal, and limestone. Some of them appear to be metalliferous, but as they have been placed in the hands of a competent gentleman for the purpose of being analyzed, whose report is shortly expected, it is unnecessary at present to hazard an opinion as to their specific qualities. We estimated the distatice from Mr. Brockman's house to the river which washes the base of the Dyott Hills, and which formed the extreme point or termination of our journey, to be forty miles in due easterly course, and to which there is no obstacle of sufficient importance to prevent a good communication from being opened. The general characteristic of the soil of the country to the eastward of Mount Mackie, which we considered to be the eastern extremity of Darling's Range, was a light, sandy loam, the sub-soil of which was clay, which occasionally appeared on the surface. In some places there was a rich red loam, and the banks of the last-mentioned river were principally alluvial.
(Signed) R. DALE.
