the left bank of the stream
which has been considered to be the Arrowsmith River of Captain Grey,
though I have now some reason to doubt its identity. The banks of the
stream are sandstone and sand, and the channel scarcely three yards wide,
with a strip of grassy thicket twenty yards in width along the stream,
which is the only feed near the river, as the plain through which it runs
produces nothing but scrub and banksia with a few grass-trees. We
bivouacked a short distance below the spot where we first struck the
stream, which was still running.

3rd November.

Our horses having but a very scanty feed at this place, we moved down the
stream to obtain better grass for them before crossing the sand-plains
which lay to the south. After following the stream west for two hours,
encamped in a small grassy flat, below which the stream ceased to run,
the water being wholly absorbed by the sandy soil, which has a substratum
of limestone of recent formation.

SEVENTY MILES OF SAND PLAIN.

4th November.

Accompanied by Mr. Bedart, rode to the westward; passing over sandy
plains and ridges for four hours, came to the beach, which we followed
northwards for three hours, hoping to meet with the mouth of the stream
on which our camp was placed. Not perceiving any signs of it, we turned
to the east, and after an hour's struggle through a thick jungle, we came
on a wet grassy flat, on which the stream seemed to be lost. Steering a
general course of south-south-east, we arrived at 9.10 p.m. at the camp,
after a ride of thirteen and a quarter hours, and the country traversed
almost wholly worthless sand and scrub.

5th November (Sunday).

Remained at our encampment to rest the horses. Read prayers.

6th November.

Leaving our encampment at 7.10 a.m., we steered north 170 degrees east
magnetic, along the limits of the low scrubby limestone hills which
extend along this part of the coast. To the east the level sandy plain
extended from eight to ten miles, and then rose into high sandstone
hills, covered with scrub and destitute of trees; but at the junction of
the limestone and sandstone formation, along which lay our route, were
several small lagoons and swamps of fresh water, with grassy margins. At
10.0 altered the course to southward; the line of swamps trending to
south-south-west, we entered the level sandy plain. At noon passed a
shallow pool of rainwater in a slight depression of the plain, and
shortly after crossed