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The History of Australian Exploration from 1788 to 1888 by Ernest Favenc
page 46 of 664 (06%)
Kosciusko, falling some 700 feet short of the limit of perpetual snow,
its elevation being 7,308 feet.

To the westward, many of the peaks reach altitudes of over 5,000 and
6,000 feet, until the large depression is encountered through which the
great body of interior waters find their way to the sea by means of the
Murray Channel.

West of this gap, the edge of the tableland is broken, and depressed, the
highest crests of the coastal range rarely reaching to 3,000 feet in
height, and along the shore line, facing the Great Australian Bight, it
is almost non-existent.

On reaching the south-west corner of Australia, the elevated edge reforms
in the Russell and Darling Ranges, and trending northward, skirting the
coast, culminates in Mount Bruce, 4,000 feet above sea level. From hence,
the range following the sea line is broken, rugged and precipitous, but
of inconsiderable height, and when the centre of the Gulf of Carpentaria
is reached, it falls away into highlands and slopes, joining the eastern
ranges.

On the great plateau encircled by this range, no elevations of any moment
are to be found; a kind of chain traverses the centre from north to
south, but though in places presenting a bold formation, the highest
altitude attained is in the Macdonnell Ranges--4,000 feet.

From the coastal range, the edge of the tableland, flow the rivers that
run direct to the sea on the seaward face; but in many instances a false
tableland occurs, the streams that drain which unite in forcing their way
through deep gorges to the lowlands of the coast. This false tableland is
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