- We proceeded north by west to latitude 19 degrees 32 minutes,
and crossed several gullies coming from the basaltic ridges:
These,
however, receded far from the river, and large box and Ironbark flats
took their place for about three miles, when the ridges re-appeared.
Between four and five miles from the bar of red rock above mentioned, a
fine large creek joined the Burdekin from the westward. The box and
Ironbark forest was interrupted by slight rises of limestone full of
corals; and by a higher hill of baked sandstone, at the foot of which a
limestone hill was covered with a patch of Vitex scrub. The strata of the
limestone seemed to dip to the southward.
The opposite banks of the river were ridgy, but openly timbered, and this
fine country, with its well grassed flats, and its open ridges, seemed to
extend very far on both sides. Messrs. Gilbert and Roper went to the top
of the hill, and saw ranges trending from west to north, with that
crenelated outline which I had before seen and mentioned: they
distinguished a large valley, and the smoke of several fires of the
natives along the range. A large lagoon was at the western foot of the
hill on which they were. A large creek was seen, by Brown, to join the
Burdekin from the north-east, at a short mile from our encampment. A
baked sandstone and pudding-stone of a white colour projected into the
river at the place, which not only exhibited the transition from one rock
into the other, but it showed the action of igneous rocks on both, and
gave a clue to the nature of the red rock I described yesterday.
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