Cowboy Tin Mine
Hill City, South Dakota
43.9277°N 103.5977°W
43.9277°N 103.5977°W
The Cowboy Tin Mine is near Hill City, South Dakota. Historically the site has been associated with the Hill City Mining District which is now part of the Black Hills National Forest. The site was first discovered in 1884. The Cowboy Tin Mine was closed at the time of data entry with no known plans to re-open. Mine operations consist of underground workings. Underground features include 2 shafts and 1 incline. Subsurface depth reaches a maximum of 61 meters (200 feet) and extends 2,000 meters (6,562 feet) in length. The mining method is shrinkage methods. Documentation from 1981 describes a single ore body as having a lenticular or lens shaped form reaching 46 meters (150 feet) long, 1 meter (2 feet) wide, and 61 meters (200 feet) thick. The Black Hills of the Interior Plains characterize the geomorphology of the surrounding area.
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Other deposits in the same region.
Cowboy Lodes Tin Mine
Campaign Tin Occurrence
Coats Dike Tin Mine
Coats Claim
Unnamed Tungsten Occurrence
Wolfram Lode
Annie Lode
Tin Chance Tungsten Prospect
Tin Spike Mine
Gertie Tin Mine
* 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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Deposit
REFER TO FIGS 1-3 (WMR 377 ), FIGS 11+12 (PP 247, P 93-4) AND (IC 7069) FOR PLAN AND SECTIONAL VIEWS OF COWBOY TIN MINE. RESERVE ESTIMATES MADE BY BUR OF MINES STAFF (WMR 377, P 6) SH TONS AT 0. 46 SR AND 640 SH TONS BROKEN ORE IN STOPES. TONS ADDED TO TOTAL FOR INFERRED. COWBOY DEPOSIT IS A WELL-DEFINED PEGMATITE-QUARTZ-MUSCOVITE-CASSITERITE VEIN. CASSITERITE OCCURS IN A GREISEN-TYPE VE WITHIN THE PEGMATITE. THESE CASSITERITE SEAMS ARE OF SHOR ICAL AND HORIZONTAL DIMENSIONS AND ARE IRREGULAR IN OCCURR.