The accident of a drought in 1813 drove some of the Sydney settlers
to look for new pastures in the hinterland. The divide between the
short eastward and the long westward drainage systems was surmounted
with difficulty; a road to the point where the town of Bathurst
afterwards grew up was promptly made, and an arresting geographical
problem confronted the investigators when the westward-flowing rivers
Macquarie and Lachlan were found. Lieutenant Oxley, R.N., attempting to
follow the Lachlan in 1815, was presently brought to a halt by great
swamps. He struck south to avoid them, and narrowly missed discovering
the Murrumbidgee river, before he turned back to carry to Sydney the
conviction that the westward drainage generally was lost in swamps
fringing an inland sea. Cunningham found a route from this coast up
to the rich Liverpool Plains, towards the north of New South Wales,
in 1823; but for the most part exploration was temporarily directed
to the south-west, and Hamilton Hume and Hovell in 1824–25 took an
inland route from New South Wales to the south coast on the west side
of Port Phillip. This inlet was not recognized by them; they returned
to report that they had seen the coast-land, and found it good, further
to the east at Western Port; settlers who visited that district on
their recommendation were disappointed, and the development of the
Victoria coast-lands received a set-back in consequence of this error.
Cunningham in 1828 opened the route from the coast at Brisbane to the
downs of the south Queensland hinterland. In the same year a new phase
was entered in the solution of the problem of the far interior, when
Charles Sturt, carrying with him Oxley’s conviction of the existence
of an inland sea, journeyed inland at a season of drought to find
the Macquarie river losing itself on the dry plains, and the Darling
flowing salt. He attributed this fact to an admixture of sea-water, and
set down the interior of the continent as a desert. In the following
year he settled the problem of the drainage of the Murrumbidgee,
Lachlan, and Murray rivers by following them to the mouth of the Murray
in Lake Alexandrina (south coast); and although he now held that the
waters of the Darling were included (as they are) in this system, it
was still doubted whether there was a divide between north and south
flowing waters about the central latitude of New South Wales, where,
in the interior, high ground was known to exist. Sir Thomas Mitchell
settled this question by a great journey in 1836, which, among other
results, immediately threw open to settlement the fertile country
about Port Phillip, hitherto, as we have seen, neglected through the
misunderstanding of Hume and Hovell.
Public-domain text, read in full here on John Shaqi.
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