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Updated: May 24, 2025


As a general rule in many parts of Australia though by no means an inflexible rule a reef running east of north and west of south will underlie east; if west of north and east of south it will go down to the westward and so round the points of the compass till you come to east and west; when if the strike of the lodes in the neighbourhood has come round from north-east to east and west the underlie will be to the south; if the contrary was the case, to the north.

But it must be understood that most auriferous lode stuff contains a proportion of sulphides of various metals, wherein a part of the gold, usually in a very finely divided state, is enclosed, and on this gold the mercury has no influence. Also many lodes contain hard heavy ferric ores, such as titanic iron, tungstate of iron, and hematite, in which gold is held.

So the surface gold in the alluvium deposits was all that was collected by the Spaniards, and what there still may be on the bed-rocks of the rivers or in the lodes in the mountains from which it has been washed, awaits the advent of modern gold-seekers.

The case is similar to that of the rotation of crops in its relation to scientific microbiology. The art of mining may get ahead of the science of physiography in respect of earth-currents and lines of least resistance, as showing where mineral lodes may be expected. Yet there is no doubt whatever that science will not in the one case lag so far behind as it has done in the other.

The trend of the main ranges, also nearly east and west, is probably due to the direction of the outcrops of the lodes which have resisted the action of the elements better than the soft dolerytes. The quartz veins now form the crests of many of the ranges, but are everywhere cut through by the lateral valleys.

In this work he was ably assisted by Secretary Jack Muddle, who became quite celebrated as a clear expounder and explainer of veins, lodes, ores, cross-cuts, shafts, levels, winzes, minerals, metals, and mines insomuch that he was regarded by many of the confiding public who frequented his office as a more thoroughly learned and scientific man than George Augustus himself.

Many of the miners had claims on several different lodes, and although they might have faith in their richness, they wanted to sell part of them to get means to work the rest.

"What dost mean by these words, lodes? how have I ever shown that I have forgotten thee? Dost expect me, who have my studies to employ me, and my future to consider dost expect me to come philandering here on the cliffs after a shepherdess?" "No," said Morva, trying to curb her hot Welsh temper, which rushed through her veins, "no! I only ask you to free me from my promise.

But as in Nature's laboratory the processes, if certain, are slow, this theory may be difficult to prove. Why the junction of lodes is often found to be more richly metalliferous than neighbouring parts is probably because there the depositing reagents met. This theory is well put by Mr. S. Herbert Cox, late of Sydney, in his useful book, "Mines and Minerals."

Ordinary metalliferous Veins or Lodes. Their frequent Coincidence with Faults. Proofs that they originated in Fissures in solid Rock. Veins shifting other Veins. Polishing of their Walls or "Slicken sides." Shells and Pebbles in Lodes. Evidence of the successive Enlargement and Reopening of veins. Examples in Cornwall and in Auvergne. Dimensions of Veins.

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