At 8 O'clock
P.M. A Fine Strong Northerly Breeze Came Up The River, Flowing Along Its
Broad Open Valley, And Which I Supposed To Be The Sea Breeze.
This
supposition was somewhat confirmed by a similar breeze occurring at the
same time on the following evening.
The plains are basaltic, and occasionally covered with pebbles of white
and iron-coloured quartz and conglomerate, and are in the vicinity of
slight elevations, which are probably composed of sandstone and
conglomerate, and usually covered with low scrub and cypress-pine.
Sandstone crops out in the gullies of the valley, in horizontal strata,
some of which are hard and good for building, others like the blue clay
beds of Newcastle, with the impressions of fern-leaves identical with
those of that formation. At the junction of Comet Creek and the river, I
found water-worn fragments of good coal, and large trunks of trees
changed into ironstone. I called this river the "Mackenzie," in honour of
Sir Evan Mackenzie, Bart., as a small acknowledgment of my gratitude for
the very great assistance which he rendered me in the preparations for my
expedition. Farther down the river, the country became better watered,
even at a distance from the river; some small creeks, winding down
between scrubby sandstone hills, were full of water, and a chain of fine
lagoons was crossed, covered with splendid blue Nymphaeas. Large coveys
of partridge-pigeons rose from the burnt grass as we passed along, and
ducks and pelicans were numerous on the stretches of water in the bed of
the river.
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