I Called The South-West
Branch The "Clarke," In Compliment To The Rev.
W. B. Clarke of Paramatta,
who has been, and is still, most arduously labouring to elucidate the
meteorology and the geology of this part of the world.
About three miles
above the junction, a creek of considerable size joined the Burdekin from
the northward. Wherever the ridges approached the banks of the river,
gullies which were scrubby at their heads, became numerous. After having
encamped, I rode over to the "Clarke," to examine the intervening
country. The flat along the Burdekin was about two miles and a half
broad, and was skirted by silver-leaved Ironbark ridges. In approaching
the Clarke, we came to a low basaltic range, which bounded its fine broad
openly timbered valley to the northward. The bed of the river was formed
by talc-schiste, in strata, the strike of which was from north by west to
south by east, standing almost perpendicular, with a slight dip to the
eastward. The stream was perpendicular on the line of striking. The
pebbles in its bed were mostly basaltic, baked sandstone, conglomerate,
quartz, sienite, and porphyry. I had observed the valley of this river
from a high hill near our last camp, and had distinguished many
headlands, which I now think were the bluff terminations of lateral
basaltic ranges. The valley was bounded on its southern side by a long
low range.
The blue mountain parrot was very frequent near our camp.
I have mentioned a small round eatable tuber, which I found in the basket
of a native gin on the 2nd January.
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