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Updated: June 14, 2025
The Dumot river, another mountain stream, joins the Morumbidgee opposite to Mr. Whaby's residence. It is little inferior to the latter either in size or in the rapidity of its current, and, if I may rely on the information I received, waters a finer country, the principal rock-formation upon it being of limestone and whinstone.
The face of the hill was very stony, and I found, on examination, that a great change had taken place in the rock-formation, the granite ranges having given place to chlorite schist. We reached Whaby's about 9 a.m. of the morning of the 27th, and received every attention and civility from him.
One of these valleys extended to to the S.W., the other to the W.N.W. It was evident to us that our route lay up the former; and I made no doubt we should easily reach Whaby's station on the morrow. We were now far beyond the acknowledged limits of the located parts of the colony, and Mr. Whaby's station was the last at which we could expect even the casual supply of milk or other trifling relief.
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