Pyrenees Gold Field

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I found no evidence anywhere during my rambles of " heads" or "floors " in sandstone being directly associated with rich deposits of golden stone, but the gold and quartz occur in the slates, in the main lines of drainage therein, in the minor tributary lines of drainage, and on small or large bumps on the floors or foot-walls of lodes. The thicker the seam (or so-called " make") of quartz, the greater the quantity of gold and of sulphides of lead, zinc, and iron.
The greater the quautity of gold, however, the greater is the area drained. Some layers of slate appear to be saturated with metallic ingredients in certain situations, which are rendered favorable to rich depositions by cross catchments that have long lines of slate abutting on them ; the lode at such points contains patch after patch of quartz strung together by gold.
I noticed, however, that the richest stone is always just off the line of drainage, there being a thin layer or sheet of ferruginous material deposited along the said line of direct circulation. This feature bears out the assumption that obstruction to the downward descent of solutions is the main factor in allowing them the necessary time to deposit their loads, the actual precipi­tating agents being present everywhere.
Several very rich situations in the so-called north and south' lodes in this district have been met with, outcropping, or nearly so ; one is known as the Slaughter-house lode, and from it, it is said, gold equalling 100 ounces to the ton of quartz has been mined.
I noticed miners at work on this lode, which is in" the same belt of slates as is the Moonambel formation ; the miners were trying to locate another such deposit by surface scratching, but work below in the old workings would be more likely to trace the line of the lode.
The Moonambel mine has received attention from miners at intervals for many years, but the real nature of its gold-bearing deposits appears to have been hardly understood, until Mr. J. N. Dunn, wdio has much experience of the mines of Ballarat East, inspected the mine ; he grasped tlie nature of the mine, and the result is that the Moonambel Company is about to under­take extensive works below. In the meantime, stoping is proceeding from -an old shaft 100 feet deep, and a first-class 5-head mill is crushing stone, the first crushing from wdiich has just been put through for a return of 170 ozs. of gold from 113 tons. Fifty per cent, of all yields goes, how­ever, to pay off the purchase-money, viz., £3,000, to the prospectors, .Messrs. Doherty, Green, and party ; and, judging by the appearance of the present faces, the payment of this debt will be only a matter of a couple of months or so. I noticed that areas to the north-west and south-east of the Moonambel mine are under applications for lease, and that preparations for work on the same system of lodes are in progress. Moonambel is already beginning to show more activity, which should be enduring, owing to tlie rich golden ores in the mountains around it.
On the other side of the mountain range on which the Moonambel mine is situated, and on the same belt of slate, Mr. Joe Wright, an expert loamer, is tunnelling into the spur, on a " floor *' which cuts the underlay of the slate at right angles (see Plate V.). He and his two boys have followed a little seam of quartz, which lies on the floor, along the line of intersection of .same with theslate; they have gone for about 100 feet, for returns in gold which give the party about £25 per week. Here all the features which obstruct the circulation are shown in a channel in the slate about an inch wide ; it occurs at the point where it abuts on to tlie floor. Parts of the line of
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