fast one tree to top of another
tall tree, I obtained a view of the horizon, which appeared perfectly
level, and I was in hopes that we had at length found a river which
would flow to the northward and avoid the Darling. I accordingly
ordered the boat to be put together, and sent Mr. White with a party
some miles down to clear away any trees in the way. Mr. White came upon
a rocky fall, and found besides the channel so much obstructed by
trees, and the course so tortuous, that I determined to ascertain
before embarking upon it, whether the general course was in the desired
direction. Leaving Mr. White with half the party, I accordingly traced
the Karaula downwards, and found that its course changed to south, a
few miles below where I had made it, and that it was joined by the
Gwydir only eight miles below where I had crossed that river.
Immediately below the junction of the Gwydir (which is in latitude 29
degrees 30 minutes 27 seconds, longitude 148 degrees 13 minutes 20
seconds) the course of the river continues southward of west, directly
towards where Captain Sturt discovered the River Darling; and I could
no longer doubt that this was the same river. I therefore returned to
the party, determined to explore the country further northward.
The results of my progress thus far were sufficient, I considered, to
prove that the division of the waters falling towards the northern and
southern shores of Australia is not, as has been supposed, in the
direction of the Liverpool and Warrabangle range, but extends between
Cape Byron on the eastern shore, towards Dick Hartog's Island on the
west; the greater elongation of this country being between these
points, and intermediate between the lines of its northern and southern
coasts. The basin of the streams I have been upon must be bounded on
the north by this dividing ground or water-shed, and although no rise
was perceptible in the northern horizon, the river was traversed by
several rocky dykes, over which it fell southward; their direction
being oblique to the course, and nearly parallel to this division of
the waters. I beg leave to state, that I should not feel certain on
this point without having seen more, were it not evident from Mr.
Cunningham's observations, made on crossing this division on his way to
Moreton Bay. Mr. Cunningham, on crossing the head of this river, nearly
in the same latitude, but much nearer its sources, found the height of
its bed above the sea to b
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