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Y MEANS OF TWO DISHES, AND A TRIPOD STAND AND PULLEY. A tripod, twelve or fifteen feet high, is set up over a hard and smooth piece of ground. By a rope and pulley the full dish is hauled up as far as required; the rope is then made fast and a string, fixed to the edge of the dish, is pulled, and the dish tipped up allowing the dirt to fall on to the prepared surface below, where it is swept up and treated as in the first method described. With a fair breeze this is a very effectual way of getting rid of the fine dirt. 3 BY MEANS OF A SIEVE. This method is only suitable when the soil is wet and sticky, or where the nuggets are fairly large and not too rare. On the first rush to Kurnalpi, where more alluvial gold was found in a short time than on any other field, sieves were almost the only implements used. A sieve is very useful for prospecting the surface soil, being more portable and more rapidly worked than the dishes. A combination of these three methods is found in the DRY BLOWING MACHINE. It has always been a hotly debated question, whether what is known as the "Cement" comes under the heading of "reefs" or "alluvial." This cement is composed of angular quartz-fragments, broken from the reefs or veins, and fragments of diorite and hornblende schists, cemented together by lime; it is very hard and solid and, in places, continues to a depth of over twenty feet. The gold is extracted from these depths by crushing and dry-blowing. I have mentioned this peculiar composition last, as I am not at all clear to which class of formation it belongs. At first this cement, which the shallow alluvial ground overlies, was supposed to be "bottom," that is to say, that there was considered no likelihood of gold being found at a greater depth. Later developments, however, have proved this theory to be wrong, and with regard to this I cannot do better than quote extracts from a report made by Mr. E. P. Pittman, Government Geologist of New South Wales, in which he says:-- "He had considered the question of deep-leads of alluvial, and after visiting Coolgardie, Kalgoorlie, and Kanowna, he thought it probable that there would shortly be a large output of alluvial gold from this source. In Coolgardie the dry-blowing had been confined to a very shallow depth, and yet close to Coolgardie--in Rollo's Bore--there was evidence of the existence of a very deep valley. He produced a specimen, taken by him from an alluvial wor
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