Mary Orndorff Prospect
Maurertown, Virginia
38.9881°N 78.5341°W
38.9881°N 78.5341°W
The Mary Orndorff Prospect is near Maurertown, Virginia. Historically the site has been associated with the Cedar Creek Valley Mining District which is now part of the George Washington National Forest. The ore mined is composed of pyrolusite with waste material consisting primarily of chert. 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.
2. 4 KM (1. 5 MI) SOUTHWEST ON STATE ROAD 713 FROM ITS INTERSECTION WITH STATE ROAD 600, PROSPECT IS 170 M (558 FEET) SOUTHEAST OF 713 ALONG THE CREST OF THE RIDGE. ADDITIONAL WORKING AT UTM N 4317985, E 713390, ZONE +17.
Formal or informal mining district names.
A 5 M (16 FEET) SHAFT WAS SUNK ON THE UPPER NORTHWEST SLOPE OF THE RIDGE AND A NEARBY OPEN CUT WAS DUG ON THE CREST OF THE RIDGE. THE SHAFT WAS SUNK IN THE NEW SCOTLAND LIMESTONE AND THE OPEN CUT IS IN THE RIDGELEY SANDSTONE. IN 1982, A CAVED PIT (SHAFT ), ABOUT 3M (10 FEET) IN DIAMETER, ON THE SOUTHEAST SIDE OF THE CREST AND A SMALL TRENCH, 3 M (10 FEET) LONG, 1 M (3 FEET) WIDE, AND 0. 6 M (2 FEET) DEEP, ALSO ON THE SOUTHEAST SIDE OF THE CREST, WERE EVIDENT. AN OLD FARM ROAD CROSSES THE CREST A SHORT DISTANCE BELOW THE PIT AND IT MAY PASS THROUGH THE OLD OPEN CUT.
FOR GEOLOGY SEE YOUNG AND RADAR (1974).
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.
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Ralph Orndorff Prospect
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Ralph Orndorff Prospect
Ralph Orndorff 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
WORKINGS EXPOSED CHERT AND SANDY CLAY WHICH YIELDED A SMALL QUANTITY OF MANGANESE OXIDE IN WHICH THERE WAS CONSIDERABLE SAND. THE MANGANESE OCCURS MOSTLY AS A CEMENT AND STAIN IN THE SANDSTONE.