Caldwell Barium Prospect
Fincastle, Virginia
37.4956°N 79.9364°W
37.4956°N 79.9364°W
The Caldwell Barium Prospect is near Fincastle, Virginia. Historically the site has been associated with the Roanoke-Botetourt Counties Area which is now part of the Jefferson National Forest. The site was first discovered before 1938. Mine operations consist of surface workings. There is one known shaft. The ore mined is composed of sphalerite and barite with waste material consisting primarily of limestone, shale and dolomite. The ore body is described as having an irregular shape of unknown dimensions. The host rock in this area is limestone. The Middle Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
Additional textual information about a site or mine.
1. 8 KM (1. 1 MI) WEST ON STATE ROAD 600 FROM ITS INTERSECTION WITH STATE ROAD 670, SOUTHWEST OF HOWELL MILLS; 290 M (951 FEET) SOUTH OF ROAD ON THE CREST OF A HILL.
PROSPECT WAS WORKED BEFORE 1938 AND THE WORKINGS CONSIST OF 8-12 OPEN PITS AND TRENCHES. THE WORKINGS WERE HAND DUG AND THEY STRIKE N 50 DEG E FOR ABOUT 91. 5 M (300 FEET).
Workings at the site.
8-12 OPEN PITS AND TRENCHES WERE DUG, SIZES VARIED, BUT THE LARGEST TRENCH WAS 6 M (20 FEET) LONG, 3 M (10 FEET) WIDE, AND 2. 4 M (8 FEET) DEEP.
EDMUNDSON (1938) DESCRIBES THE PROSPECT TO BE IN ATHENS SHALE. MORE RECENT WORK INDICATES THE DEPOSIT OCCURS IN LIMESTONE AND DOLOMITE OF THE LINCOLNSHIRE FORMATION AND THE SURROUNDING SHALE (ATHENS) IS PART OF THE EDINBURG FORMATION. THE CONTACT BETWEEN THESE TWO FORMATIONS IS VERY CLOSE TO THE DEPOSIT. FOR A GEOLOGIC MAP OF THE AREA SEE MCGUIRE, O. S ., 1976, GEOLOGY OF THE DALEVILLE QUADRANGLE, VIRGINIA: VIRGINIA DIVISION OF MINERAL RESOURCES REPORT OF INVESTIGATIONS 42.
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.
Controls on emplacement of ore such as faults or other structural features.
Other deposits in the same region.
Gusler-Austin Mine
Unnamed Iron Prospect
Maude Hematite Mine
Unnamed Manganese Prospect
Unnamed Manganese Prospect
Daleville Opening Iron Prospect
Unnamed Manganese Prospect
Troutville Lead Prospect
Troutville Lead Prospect
Unnamed Manganese Prospect
* 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
PITS CONTAIN FRACTURED LIMESTONE AND DOLOMITE AND ATHENS SHALE OUTCROPS ALL AROUND THE SITE. BARITE IS DARK GRAY TO BLACK IN COLOR, CONTAINS CARBONACEOUS MATTER, AND SMELLS OF H2S WHEN RUBBED BY ANOTHER PIECE. THE PROSPECT OCCURS JUST SOUTH OF A FAULT TRACE.