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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.
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.
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.
At the head of the valley we crossed a small dividing range into another valley, and halted for the night, on the banks of a creek from the westward, as we found it impossible to reach Whaby's station, as we had intended, before sunset. Nothing could exceed the luxuriance of the vegetation in this valley, but the water of the creek was so impregnated with iron, as to be almost useless.
The rock formation of the hills upon its right continued of that chlorite schist which prevailed near Mr. Whaby's, which I have already noticed, and quartz still appeared in large masses, on the loftier ranges opposite, so that the geology of the neighbourhood could not be said to have undergone any material change.
It will be needless to follow the progress of the party through the settled districts that now extended to the banks of the Morumbidgee: on the 27th, we find them preparing to start from Mr. Whaby's station, the last outpost of civilization. From thence they followed the river down, maintaining constant and friendly intercourse with the natives on the banks.
At the head of the valley we crossed a small dividing range into another valley, and halted for the night, on the banks of a creek from the westward, as we found it impossible to reach Whaby's station, as we had intended, before sunset. Nothing could exceed the luxuriance of the vegetation in this valley, but the water of the creek was so impregnated with iron, as to be almost useless.
The rock formation of the hills upon its right continued of that chlorite schist which prevailed near Mr. Whaby's, which I have already noticed, and quartz still appeared in large masses, on the loftier ranges opposite, so that the geology of the neighbourhood could not be said to have undergone any material change.
On the following morning, we started for the place at which it had been arranged that we should cross the Morumbidgee, but, though no more than five miles in a direct line from Whaby's house, in consequence of the irregularity of the ground, the drays did not reach it before noon. The weight and quantity of our stores being taken into consideration, the task we had before us was not a light one.
On the following morning, we started for the place at which it had been arranged that we should cross the Morumbidgee, but, though no more than five miles in a direct line from Whaby's house, in consequence of the irregularity of the ground, the drays did not reach it before noon. The weight and quantity of our stores being taken into consideration, the task we had before us was not a light one.
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