- The party moved on about ten miles to the north-east, and
encamped at the junction of a large creek which comes from the S.S.E. Its
character is similar to that of the Suttor; and I should not be surprised
if it should prove to be the northern anabranch of that creek, and which
we crossed on the 17th of March, the day before we arrived at the lake.
The country opens into lightly-timbered ridges, which are composed of a
hard rock, the sharp pieces of which covered the ground, and made our
animals foot-sore. It seems to me to be a clayey sandstone (Psammite)
penetrated by silica. A coarse-grained sandstone and quartzite cropped
out in that part of the river situated between the two camps. The
melon-holes of the box-flats were frequently over-grown with the
polygonaceous plant, mentioned at a former occasion; and the small scrub
plains were covered with a grey chenopodiaceous plant from three to four
feet high. The stiff-leaved Cymbidium was still very common, and two or
three plants of it were frequently observed on the same tree; its stem is
eatable, but glutinous and insipid.
The morning of Easter Sunday was very clear and hot; the wind from E.N.E.
As soon as we had celebrated the day with a luncheon of fat damper and
sweetened tea, I rode with Charley about seven or eight miles down the
river, and found abundance of water, not only in the bed of the river,
but in lines of lagoons parallel to it.
