Geology Of The Royal-Mountain King Hodson District, Calaveras County, California Mine

Society for Mining, Metallurgy & Exploration
T. O. Kuhl
Organization:
Society for Mining, Metallurgy & Exploration
Pages:
12
File Size:
7665 KB
Publication Date:
Jan 1, 1989

Abstract

The Royal-Mountain King Project is 7.2 kilometers (4.5 miles) northwest of Copperopolis, California. Reserves of 8,250,000 t (9,100,000 st) at 2.32 g/t (0.068 oz/st) gold will be processed at 2500 t/d (2750 st/d) from three pits. Production is scheduled to begin the first quarter of 1989. District geology consists of northwest trending sequences of Jurassic meta-sedimentary and meta-volcanic rocks. Three ore bodies are located along the Hodson fault which trends northwest and dips 40 degrees northeast. The Gold Knoll and North Pit ore bodies are hosted in carbonate and silica altered meta-volcanic rocks whereas the Skyrocket ore body is hosted in quartz stockwork zones in meta-sedimentary rocks. Gold is present as inclusions and micro-veinlets in pyrite.
Citation

APA: T. O. Kuhl  (1989)  Geology Of The Royal-Mountain King Hodson District, Calaveras County, California Mine

MLA: T. O. Kuhl Geology Of The Royal-Mountain King Hodson District, Calaveras County, California Mine. Society for Mining, Metallurgy & Exploration, 1989.

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