The object which I had then in view, with the concurrence of the Governor, was to carry the western road along the valley of the Grose, and by cutting a tunnel of about a mile through a ridge at the head of it, to reach the vale of Clywd, and so avoid the mountains altogether. The ascent to them from Emu, and the descent from them at Mount York, were both then extremely bad; so much so indeed, at the latter pass especially, that a grant of land was publicly offered by the Government to whoever could point out a better. Both these obstacles have since been overcome.
PASS OF MOUNT VICTORIA.
The pass of Mount Victoria, named by me after the youthful Princess and opened by Governor Bourke in 1832, descends at an inclination of 1 in 15 (where steepest) and avoids the abrupt descent by Mount York.
ADVANTAGES OF CONVICT LABOUR.
The new road from Emu plains, which is still less inclined, has been made during the government of Sir Richard Bourke, and relieves the Bathurst teams from the difficulties of Lapstone hill, the ascent of which cost them a whole day. The value of convict labour to a young colony is apparent in these new passes, cut in many places out of the solid rock; and this advantage will be permanently recorded in these works and others now going forward in different parts of this mountain road, which must finally make it one of the best in the colony.
COUNTRY OF MULGOEY.
The difference between the lower country on the Hawkesbury and the region which I have endeavoured to describe is very striking. The rocks are also different, for on the side of Cumberland they consist of trap, and on the other or that of the mountains, of sandstone.
EMU PLAINS.
The course of the Hawkesbury above Emu plains presents a singular feature in forcing its way through a very steep-sided ravine, and thus cutting off a portion of the mountain mass after its channel has previously bordered on the lower country of Cumberland where no such obstruction is opposed to its waters, which might there pursue a more direct course to the sea. The river takes this remarkable turn near the junction of the Nepean, and there we find in the bed of the stream (at Cox's Basin) a dark-coloured trap-rock, apparently containing steatitic matter, and doubtless connected with one of the disturbing operations to which this fractured country has been exposed.
Beyond the ferry the road crosses Emu plains, a level tract, here about a mile in width, and intervening between the river and the base of the mountains. This flat consists chiefly of gravel--composed of large pebbles, for the greater part quartzose; and in sinking a well, a bed of them was found in which many were nearly spherical.