Journal of an Expedition into the Interior of Tropical Australia, in Search of a Route from Sydney to the Gulf of Carpentaria (1848)Mitchell, T. L. (Thomas Livingstone)
History
Journal of an Expedition into the Interior of Tropical Australia, in Search of a Route from Sydney to the Gulf of Carpentaria (1848)
Mitchell, T. L. (Thomas Livingstone)
New South Wales -- Discovery and exploration; Queensland -- Discovery and exploration
28TH AUGUST.--The cattle were well refreshed by the grass on the plain: a
fresh growth was now apparent in it. We continued to travel due southward
over the plain, and through a brigalow scrub beyond it, until we crossed,
for the last time, the little river that had led us so far astray. Just
beyond it, we joined our old track, at about five miles short of Camp
LIII., to which we proceeded, and where we again encamped, although the
pond we formerly found there had dried up. We afterwards found a good
supply, at a lagoon about half a mile lower down; from which a little dog
of mine (called Procyon), had come out wet, and so made it known to us.
Thermometer, at sunrise, 40 deg.; at noon, 81 deg.; at 4 P.M., 76 deg.; at 9, 49 deg.;--
with wet bulb, 41 deg..
29TH AUGUST.--Continuing along the old track, we this day quitted the
basin of the Belyando, and ascended those grassy slopes, and that range,
which I had formerly taken to be the water-shed of the coast rivers. We
thus crossed to the basin of another eastern river, the Nog; and, in
quitting that of the Belyando, I have to observe, that like most other
Australian rivers, it maintained a peculiar character throughout its
course, with great uniformity, even after it received tributaries
apparently larger than itself. All these lapsed into the same
concatenated line of ponds; at one place, spreading amidst brigalow
scrub, at another, forming one well-defined deep channel. For the
formation of ponds, and the retention of water, in so dry a climate, we
see here something between the ordinary character of rivers, and
artificial works which man must construct, when population may spread
into these regions. The fallen timber of the brigalow decays very slowly,
and is not liable to be burnt, like most other dead wood in open forests,
because no grass grows amongst the brigalow, as in open forests. The
accumulations of dead logs become clogged with river rack and the deposit
of floods; to which floods these heaps present obstructions, forcing the
waters into new channels, and, in their progress, scooping out new ponds,
and completing the embankment of dead logs; which thus form natural dams
and reservoirs to hold, under the shade of the brigalow trees, more water
for a longer time than any single river channel could retain, however
sluggish its course. Thus it was, that during a season of unusual
drought, we had found abundance in this river's course, across nearly 31/2
degrees of latitude. The fallen brigalow presents awkward obstructions to
wheel carriages; and, as the river spreads into broad plains, and is very
favourable to the growth of brigalow, the difficulty of travelling along
this river is greatest, where its waters are most scattered. Experience
has taught us, in such cases, to endeavour to follow the river channel as
closely as possible (the general course being very straight); and thus,
open grassy spots and small plains are frequently met with, beyond which
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account