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Clunes Gold Field

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is composed of large blocks of stone, of an irregular shape, which form part of a lode line between two arches of the rock-beds. The strata form a V-shape along its line, and the lode fills a fracture that goes down vertically through the trough of an inverted arch. Other lines of cracking containing quartz makes join this main line of cracking from the east and west, as shown in Fig. 6.
Fig 6.—Sketch section showing structure of the Armagh lode, Bloomiield. Scale, about 20 feet to the inch.
These lines are evidently legs from arches to the east and west of the main lode. The prospectors have opened works on one of these side veins, which, though small, shows gold freely. There is the usual dyke material associ­ated with this lode and also the gold-slate. Old works, principally on the main body, but not exceeding 50 feet in depth, show that great quantities of material have been put through the mill from it. In addition to the main body of lode stuff, there is no telling what may be met with to the east and west of it in leg " makes " from other arches. Its outcrops, with those of other lines of lode parallel to it to the east and west, can be traced away into the deep ground of Allendale to the north, and south through the high ranges of sedimentary rock to the east of Creswick. Only one point of outcrop, other than the Armagh point, has been opened and sampled. This was at a point known as the Working Miners' mine, immediately east of Creswick, where a main shaft is down, I believe, 300 feet. Yields obtained varied between 2 dwts. and 30 dwtsv but a want of system in mining, and a want of big facilities for crushing ore, led to failure on more than one occasion. I hear that this Working Miners' mine has lately been taken up again, and that its lode formations are to receive the treatment they deserve.
In Creswick, on the Indicator belt of country which comes north from Ballarat, a lode formation known as the Nuggety has been worked occasionally by small companies during the last 30 years. The quartz occurs here in large and small irregularly-shaped "makes," nearly vertical and running, as do all the lodes of the district, nearly north and south. These formations have wing-like thin formations of quartz running out from their sides, and at points where lines of vertical drainage intersect these flat veins nuggety gold is frequently met with exactly as is the case with the flat veins of quartz in Ballarat East. One of the nuggets found here at 80 feet down turned the scale for, I believe, 126 ozs. The large blocks of stone carry gold, also, when associated with slate, and one of these, 20 feet in width, yielded an average of 7 dwts. to the ton, while another, taken from 8 feet width, yielded 18 dwts. per ton. This mine has also been acquired by a company, and new works are to be proceeded with immediately.
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Bradford. The Clunes Gold-Field.
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