Tip Top Mine
Custer, South Dakota
43.7155°N 103.6697°W
43.7155°N 103.6697°W
The Tip Top Mine is near Custer, South Dakota. Historically the site has been associated with the Custer Mining District which is now part of the Black Hills National Forest. The site was first discovered in 1880 by William Nevin. The Tip Top Mine was closed at the time of data entry with no known plans to re-open. Production size when active was considered to be small. Mine operations consist of surface and underground workings. There is one known shaft. Subsurface depth reaches a maximum of 12 meters (40 feet). The ore mined is composed of amblygonite, muscovite and beryl with waste material consisting primarily of cleavelandite, apatite and purpurite. The ore is found in dikes 60 meters (200 feet) in width. The mineralization at this location is from the Neoproterozoic era 1.00 to 0.54 billion years ago. The Black Hills of the Interior Plains characterize the geomorphology of the surrounding area.
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Additional textual information about a site or mine.
Workings at the site.
THERE ARE TWO CUTS DRIVEN NORTH. ONE (35 X 15 FEET) HAS A SHAFT 35 FEET DEEP WITH SHORT DRIFTS.
Characteristics of the ore body.
Geological materials at the site.
Geologic structural features affecting or characterizing the site or mine.
Physiographic area where the resource is found.
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* 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
ONE UNPATENTED CLAIM. GIANT CRYSTALS OF POTASH FELDSPAR ARE CONCENTRATED NEAR THE CENTRAL PORTION OF THE PEGMATITE. PEGMATITE IS COARSE TO VERY COARSE GRAINED. NOT ZONED.