Papers - Gold and Silver Milling and Cyaniding - Cyanidation at Kirkland Lake

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Donald F. Irwin
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
14
File Size:
1073 KB
Publication Date:
Jan 1, 1935

Abstract

Amid the violent economic changes of recent years that have affected Canadian gold-mining operations so deeply, the discovery and early developments of Kirkland Lake might easily be overlooked. There was more than one "false dawn" for the district before developments finally established the fact of a superb mineralized zone extending through the present operating properties. Never far from the railway, Kirkland Lake has had the benefit of direct rail service for many years. The pioneer discovery on which the first mill and cyanide plant was erected was the "Tough-Oakes," this property being on what is now the eastern end of the producing area; some time later, the "Lake Shore" was discovered at the present center of the district, and a small plant was built upon it also. Both of these early treatment plants were of pre-war design. Progress in gold metallurgy has caused a gradual change in cyanide practice since the early days at Kirkland Lake, which may be observed in the various plants now operating there. From the beginning, it was recognized that Kirkland Lake ores were more responsive to cyanidation than to alternative recovery methods, and that their mineralization contained gold in very finely divided form. Although sulfides and tellurides are present, the quantity is small, being in the order of 1 or 2 per cent by weight, so that gravity concentration is undesirable, since gold is not confined to the sulfides. Some complication is offered by the presence of tellurides, which have caused lengthy controversy over their importance in recovery methods, but which are now generally regarded as less harmful in the light of increasingly high recoveries being obtained. Nevertheless, finely divided gold intimately associated with sulfides in the presence of tellurides; and occurring in the hard Kirkland Lake porphyry ore, substantially free from natural slime-forming constituents, indicates fine grinding. This has been the universal practice although the degree of grinding has varied a little among the different mills and is considerably finer now than formerly. The natural condition as outlined caused the establishment of fine grinding at an early stage in the development of Kirkland Lake, during the period of valuation of gold at, $20.67 per ounce. With the arrival
Citation

APA: Donald F. Irwin  (1935)  Papers - Gold and Silver Milling and Cyaniding - Cyanidation at Kirkland Lake

MLA: Donald F. Irwin Papers - Gold and Silver Milling and Cyaniding - Cyanidation at Kirkland Lake. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1935.

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