THE GERALDINE LEAD MINE.

7th December.

Left our bivouac at 5.50 a.m., and steered north-east over high sandy

downs, covered with coarse scrub; at 10.30 entered the valley of the

Murchison River; at noon halted at our bivouac of the 24th September,

obtained some brackish water by digging in the sand of the small

stream-bed. Having dined, we resumed our journey at 2.30 p.m., and

bivouacked about 5.0 on the left bank of the Murchison, 500 yards below

the large lead vein, obtaining good water in the sandy bed of the river

by digging a few inches, the pools being all salt. While the men were

preparing the tents, etc., the Governor proceeded to examine the vein of

lead, which we traced to a greater distance than on the former occasion

of its discovery, the water having sunk two feet, exposing many portions

of the vein which were before covered.

8th December.

Examined the lead vein, tracing it 320 yards in a direction north 30

degrees east magnetic, along the bed of the Murchison River, which was

nearly dry; clearing the sand and loose stones from the surface, found it

to vary from eight to twenty-four inches in width, the general average

being twelve inches, the dip to the west-north-west at an angle of about

80 degrees from the horizon. Throughout the whole length the lead vein

appeared to be one solid mass of galena; the northern end either

terminates or alters its direction close to a vein of schistose rock,

which intersects the adjacent rocks; to the south the lode was covered by

several feet of sand, which prevented its being traced further, as we had

not time to remove it; the whole of the vein which was traced was

included within the banks of the river, and the greater portion was

covered by shallow water. One specimen of galena showed traces of copper.

The rock which prevails on each side of the vein is a hard compact

gneiss, abounding with garnets, some of which are of good colour, but

mostly full of flaws; the stratification of the gneiss is somewhat

confused, but it generally dips at a high angle (sometimes nearly

perpendicular) to the westward, the strike being north and south. The

facilities which the position of the lode offers for mining are not very

great, as it occupies the lowest part of the valley, and steam power

would be requisite to free the mine from water, and at the same time,

unless the small boat-harbour near the mouth of the Hutt River, or

Gantheaume Bay (both within thirty miles), be found suitable for the

purpose, Champion Bay, distant sixty-two miles in a direct line to the

south, is the nearest port where the ore could be shipped. In the evening

the Governor examined the spot where Mr. Walcott had discovered the small

pieces of lead ore about two and a half miles below the lode, but as most

of the pieces had been picked up on that occasion, we could only find a

few fragments of it.

9th December.

Left the encampment at 4.40 a.m., and steering about south-west, made our

former bivouac on the Hutt River about 1.0 p.m., and halted for the rest

of the day.

10th December.

Started at 4.50 a.m., steering 160 degrees magnetic over sandy country;

passed a small grassy valley at 8.0; halted on the north branch of the

Bowes at 10.10 on a small pool of brackish water; dined and resumed our

route at 2.40 p.m.; steered south over a grassy country till 6.10, when

we halted for the night on a tributary stream to the Bowes; obtained

fresh water by digging, the pools being very small and brackish.

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