Intial Nickel-Copper Copper Occurrence
Limestone, Montana
45.3857°N 109.9488°W
45.3857°N 109.9488°W
The Intial Nickel-Copper Copper Occurrence is near Limestone, Montana. Historically the site has been associated with the Stillwater Mining District which is now part of the Custer National Forest. The site was first discovered in 1883 by Jack Nye, Jimmy And Jonas Hedges. Ore mineralization has been found at this location and the size of the deposit is estimated to be small, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. Mine operations consist of underground workings extending 0.20 hectares (0.50 acres). There is one known shaft. The ore mined is composed of pyrrhotite, pentlandite and chalcopyrite with waste material consisting primarily of plagioclase and magnetite. The ore body is massive and disseminated in form of unknown dimensions. The host rock in this area is hornfels. The Middle Rocky Mountains physiographic province of the Rocky Mountain System characterize the geomorphology of the surrounding area.
Site identification and general characteristics. Learn about USGS mines.
Additional textual information about a site or mine.
GEOCHEMICAL ANOMALY PRESENT IN AREA OF DEPOSIT.
UNSURVEYED. IN CUSTER NATIONAL FOREST.
Workings at the site.
OLD CAVED ADIT. 787 FEET OF DRILL CORE FROM 2 HOLES DRILLED IN 1977 (ANACONDA).
Processes that concentrated or enriched the mineralization of the mine.
AGE OF STILLWATER COMPLEX IS 2, 705 +/-4 MA BASED ON U-LEAD SYSTEMATICS ON ZIRCON-BADDELEYITE (PREMO AND OTHERS, 1990).
Characteristics of the ore body.
Geological materials at the site.
Geologic structural features affecting or characterizing the site or mine.
Tectonic setting in which the site or deposit is situated.
Physiographic area where the resource is found.
Mineralogical and chemical alteration at or near the site, which may help to indicate the geographic extent of the geological processes producing the mine.
Controls on emplacement of ore such as faults or other structural features.
Other deposits in the same region.
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Mountain View Cr-Pt Platinum Occurrence
* Mine bounds on map indicate the general area that a mine occupies. For an detailed map, refer to the overseeing BLM field office.
** The mine central point is based on an average of the mine's bounding box(es) and does not necessarily fall on the claim itself.
1 World-class significance is determined by total endowment of the contained commodity. This includes all past production and remaining reserves. Each commodity is considered separately and commodities cannot be combined to arrive at a significant size. The tonnage thresholds are from the mine model grade-tonnage studies. As of June 2008, many entries were classified as significant under less strict rules.
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Notes
SEE PAGE (1979) FOR GENERAL DESCRIPTION OF BASAL SERIES MINERALIZATION. NO PUBLISHED PGE DATA AVAILABLE FOR THIS AREA.