| Deposit ID | 10106183 |
|---|---|
| MRDS ID | W031261 |
| Record type | Site |
| Current site name | Vaught, F. Mine |
| Alternate or previous names | Shaft Mine |
| Geographic coordinates: | -81.13148, 36.75536 (WGS84) |
|---|---|
| Elevation | 957 |
| Relative position | APPROXIMATELY 4.6 MILES S30E FROM SPEEDWELL ON THE SOUTH SLOPE OF IRON MOUNTAIN. |
Political divisions (FIPS codes)
Grayson(county)
Virginia(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Speedwell(quadrangle 1:24,000 scale)
Wytheville(quadrangle 1:100,000 scale)
Winston-Salem(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper New(hydrologic unit)
Kanawha(hydrologic accounting unit)
Kanawha(hydrologic subregion)
Ohio(hydrologic region)
Federal lands
Jefferson National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
George Washington and Jefferson National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Virginia | Grayson |
| Commodity | Importance |
|---|---|
| Barium-Barite Critical | Primary |
| Fluorine-Fluorite Critical | Tertiary |
| Quartz | Tertiary |
| Lead | Tertiary |
| Materials | Type of material |
|---|---|
| Barite | Ore |
| Galena | Ore |
| Quartz | Unknown |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Metamorphic Rock > Gneiss | ||||
| Rock unit name | Cranberry Gneiss Of Elk Park Plutonic Group | ||||
| Rock description | Cranberry Gneiss Of Elk Park Plutonic Group | ||||
| |||||
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Pegmatite |
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Gneiss |
| Rock unit name | Residual Clay;Cranberry Gneiss |
| Rock description | Residual Clay;Cranberry Gneiss |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Pegmatite |
| (1) | -81.13148, 36.75536 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Ne-Sw Trend, Blue Ridge Anticlinorium; E-W Trending Stone Mountain Thrust Fault Family. |
| Type of structure | Local |
| Structure description | E-W Trending Normal Fault |
| General form | IRREGULAR |
|---|---|
| Dip | 60 DEG S |
| Thickness | 1.22M |
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1927 |
| District name | Gossan Lead District |
|---|
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | Callahan, William H. |
| First year | 1986 |
| Type of workings | Surface/Underground |
|---|---|
| Overall depth | 15M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W031261 |
EDMUNDSON, R.S., 1938, BARITE DEPOSITS OF VIRGINIA: VIRGINIA GEOLOGICAL SURVEY BULLETIN 53, 85P.
STOSE & STOSE, 1957, GEOLOGY AND MINERAL RESOURCES OF THE GOSSAN LEAD DISTRICT AND ADJACENT AREAS IN VIRGINIA: VIRGINIA GEOLOGICAL SURVEY BULLETIN 72, 233P.
RANKIN, ESPENSHADE AND NEWMAN, 1972, GEOLOGIC MAP OF THE WEST HALF OF THE WINSTON SALEM QUADRANGLE, NORTH CAROLINA, VIRGINIA AND TENNESSEE, USGS MISCELLANEOUS INVESTIGATIONS MAP I-709-A.
EDMUNDSON (1938)
| Subject category | Comment text |
|---|---|
| Deposit | THIS IS THE LARGEST AND MOST EXTENSIVELY DEVELOPED PROSPECT/MINE IN THE NORTHERN GRAYSON COUNTY - FALLVILLE AREA. ; INFO.SRC : 1 PUB LIT; 3 FIELD OBSERV; 5 PERS COMM |
| Deposit | BARITE OCCURRED AS LENSES IN THE OPEN CUT AND IN THE SHAFT. THE BARITE LENS IN THE OPEN CUT WAS A SOLID MASS 1.2M (4 FT) WIDE WHICH YIELDED 20 TONS OF BARITE. BEDROCK DOES NOT CROP OUT IN THE OPEN CUT, BUT WEATHERED PINK PEGMATITE WAS ENCOUNTERED IN THE SHAFT, CONTAINING ABUNDANT BARITE, FLUORITE, AND SECONDARY QUARTZ. BARITE COLLECTEDON THE MICA DUMP WAS MASSIVE WITH CLUSTERS OF FINE GRAINED CRYSTALS, OCCASSIONALLY VUGGY AND IRON STAINED. FLOAT PIECES OF BARITE ARE UP TO 10 INCHES THICK. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1987 | Trimble, David C. (Sweet, Palmer C.) | Virginia Division of Mineral Resources | |
| Updater | 01-FEB-1987 | Lovett, James A. | Virginia Division of Mineral Resources |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.