In this place I observed and calculated three sets of lunar observations; one gave longitude 144 degrees 4 minutes, and the other longitude 144 degrees 14 minutes. As usual, we greased our harness, although not without considerable discussion, as to whether it would not be more advisable to eat the fat than to apply it to the leather; we also repaired our packs and pack-saddles, and put every thing in travelling order.
On the 29th April we started from our killing camp, and travelled about seven miles N. 70 degrees W.; making our latitude 18 degrees 59 minutes. The ranges now approached the banks of the river, and retarded our progress very much.
April 30.—In consequence of Charley’s statement, that the banks of the river in advance were so steep and rocky that it would be impossible for us to pass, I left the river side, and crossed over the ranges, and had a very heavy stage for my bullocks; which I regretted the more, as Mr. Calvert and Brown, who returned to our last camp for a sword, had found the route by the river quite practicable. The ranges were composed of a Psammite, which was frequently baked, probably by neighbouring out-bursts of igneous rock. Several familiar forms of plants were discovered; also a new Eucalyptus, with a glaucous suborbicular subcordate leaf, and the bark of the rusty gum: a stunted or middle-sized tree, which grew in great abundance on the ranges. We passed a fine large but dry Casuarina creek, coming from the westward, with a broad sandy bed. A large tree, with dark green broad lanceolate stinging leaves, grew on its banks; it resembled the nettle tree, but belonged to neither of the two species growing in the bushes of the east coast.
Our last day’s travelling had not advanced us more than five miles in a straight line, and we had not made any northing, our latitude being again 18 degrees 59 minutes; but we had left the mountains behind us, and had travelled, during the latter part of the stage, over well grassed, openly timbered flats. The ranges on the left side of the river extended several miles farther, but gradually sunk into a level country.
[Note 1: The following description of the fossiliferous limestone of the Burdekin, was communicated to me by the Rev. W. B. Clarke, F.G.S.
This rock consists of a semi-crystalline, greyish-brown marble, very like some varieties of Wenlock limestone.