Three Expeditions into the Interior of Eastern Australia, Volume 2: With Descriptions of the Recently Explored Region of Australia Felix, and of the Present Colony of New South WalesMitchell, T. L. (Thomas Livingstone)
History
Three Expeditions into the Interior of Eastern Australia, Volume 2: With Descriptions of the Recently Explored Region of Australia Felix, and of the Present Colony of New South Wales
Mitchell, T. L. (Thomas Livingstone)
Australia -- Discovery and exploration; Mitchell, T. L. (Thomas Livingstone), 1792-1855
The noise and bustle of the house was quite refreshing to one who had
dwelt so long in deserts, although it seemed to promise little
accommodation, for there had been races in the neighbourhood and horses
lay about the yard. Nevertheless the waiter and his wife cleared for my
accommodation a room which had been full of noisy people, and my horses
were soon lodged snugly in the stable. There indeed I perceived more room
than the house afforded, for while the guests were regaling within their
horses were allowed to lay about to starve outside, as if so many gypsies
had been about the place; no uncommon circumstance in Australia.
October 30.
In the course of my ride this morning I recognised the poor scrubby land
about the southern boundary of the county of Argyle, which I had surveyed
in 1828. The wood on it is rather open, consisting of a stunted species
of eucalyptus, the grass, apparently a hard species of poa, affording but
little nourishment. Sandstone and quartz are the predominant rocks
although some of the most remarkable hills consist of trap.
BREDALBANE PLAINS.
Passing at length through a gap in a low ridge of granular quartz, we
entered upon Bredalbane plains, consisting of three open flats of grassy
land circumscribed by hills of little apparent height, and extending
about twelve miles in the direction of this road, their average width
being about two miles. Deringullen ponds arise in the most southern
plain, and are among the most eastern heads of the Lachlan. The plains
are situated on the high dividing ground or water shed between the
streams falling eastward and westward, and had probably once been lagoons
of the same character as those which still distinguish other portions of
this dividing ground.
LAKE GEORGE.
The most remarkable of these is Lake George, about fourteen miles further
to the south, and which in 1828 was a sheet of water seventeen miles in
length and seven in breadth. There is no outlet for the waters of this
lake although it receives no less than four mountain streams from the
hills north of it, namely Turallo creek, whose highest source is fourteen
miles from the lake, Butmaro creek which arises in a mountain sixteen
miles from it, Taylor's creek from the range on the east, six miles
distant, and Kenny's creek from hills five miles distant. The southern
shore of this lake presents one continuous low ridge, separating its
waters from the head of the Yass river which would otherwise receive
them. The water was slightly brackish in 1828 but quite fit for use, and
the lake was then surrounded by dead trees of the eucalyptus measuring
about two feet in diameter, which also extended into it until wholly
covered by the water. In that wide expanse we could find no fish, and an
old native female said she remembered when the whole was a forest, a
statement supported pro tanto by the dead trees in its bed as well as by
the whole of the basin being in October 1836 a grassy meadow not unlike
the plains of Bredalbane.
Public-domain text, read in full here on John Shaqi.
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