A small fish, with yellow and dark longitudinal lines, and probably
belonging to the Cyprinidae, was caught. Wind prevailed from the
northward: the forenoon was cloudless; heavy cumuli in the afternoon.
We travelled at first on the right side of the river; but its banks
became so mountainous and steep, and the gullies so deep, that we were
compelled to cross it at a place where it was very deep, and where our
horses and cattle had to swim. Many of our things got wet, and we were
delayed by stopping to dry them.
April 4. - We moved our camp to latitude 20 degrees 24 minutes 12 seconds,
a distance of about nine miles N.W. by N. We passed several granitic
peaks and ranges; one of which I ascended, and enjoyed an extensive view.
The character of the country changed very little: open narrow-leaved
Ironbark forest on a granitic sand, full of brilliant leaflets of mica.
Some deep creeks came from the eastward. To the west and north-west
nothing was to be seen but ridges; but high imposing ranges rise to the
north and north-east. At one spot, large masses of calcareous spar were
scattered over the ground; they were probably derived from a vein in the
granite.
Three black ducks, (Anas Novae Hollandiae) were shot. Tracks of native
dogs were numerous; and a bitch came fearlessly down to the river, at a
short distance from our camp. Our kangaroo dog ran at her, and both fell
into the water, which enabled the bitch to escape.
April 5. - We re-crossed the river, which was not very deep, and travelled
about nine miles N. 75 degrees W. The river flows parallel to a high
mountain range, at about three or four miles from its left bank. I named
this after Mr. Robey, another friendly contributor to my outfit. A large
creek very probably carries the waters from this range to the Burdekin,
in latitude 20 degrees 23 minutes. The country was very ridgy and hilly;
and we found it exceedingly difficult to proceed along the river. We
observed the poplar-gum again in the open forest, and a fine drooping
loranthus growing on it. Pandanus was also very frequent, in clusters
from three to eight trees. The clustered fig-tree gave us an ample supply
of fruit, which, however, was not perfectly mellow.
Veins of calcareous spar and of quartz were again observed. I ascended a
lofty hill, situated about a mile and a half to the west of our
encampment, and found it composed of felspathic porphyry, with a greyish
paste containing small crystals of felspar; but, in the bed of the river,
the same rock was of a greenish colour, and contained a great number of
pebbles of various rocks, giving it the aspect of a conglomerate; but
recognisable by its crystals of felspar, and from its being connected
with the rock of the hill.
