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Updated: May 14, 2025
Below the junction of the Conadilly, where the well-known native name is the Namoi, it pursues a north-west course. The men threw in their lines, but caught during the day only two fishes, similar to those we obtained at Perimbungay. The alluvial bed of the stream consisted of marl, fragments of red quartz, and other rocks. A very hard yellow calcareous sandstone also occurred in the bank.
Lofty bluegum-trees grew on the margin of the stream, and the place, upon the whole, seemed favourable for the formation of a depot, where I might leave the cattle to refresh while proceeded down the Namoi in the canvas boats, with the materials for constructing which, we were provided. This river was the channel of the united waters of the Peel, Muluerindie and Conadilly.
This stream, having received the Conadilly from the left bank, had here an important appearance: the breadth of the water was 100 feet, its mean depth 11 3/4 feet; the current half a mile per hour, and the height of the banks above the water 37 feet. The course of the Muluerindie, from the junction of the Peel to that of the Conadilly, is somewhat to the southward of west.
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