| Deposit ID | 10105492 |
|---|---|
| MRDS ID | W000673 |
| Record type | Site |
| Current site name | Stanley Mine |
| Alternate or previous names | Eurekamine |
| Geographic coordinates: | -78.51055, 38.56004 (WGS84) |
|---|---|
| Elevation | 427 |
| Relative position | 1.6 KM (1.0 MI) SOUTH OF STANLEY. |
Political divisions (FIPS codes)
Page(county)
Virginia(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Stanley(quadrangle 1:24,000 scale)
Front Royal(quadrangle 1:100,000 scale)
Charlottesville(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
South Fork Shenandoah(hydrologic unit)
Potomac(hydrologic accounting unit)
Potomac(hydrologic subregion)
Mid Atlantic(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Virginia | Page |
| Commodity | Importance |
|---|---|
| Manganese Critical | Primary |
| Cobalt Critical | Tertiary |
| Nickel Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Manganite | Ore |
| Psilomelane | Ore |
| Pyrolusite | Ore |
| Wad | Ore |
| Limonite | Gangue |
| Result | ANALYSIS OF MN ORE: 51.46% MN, 2.94% FE, 0.23% P, 4.17% SIO2: ORE FROM 1928-1937 AVERAGED 46% MN, 3.5% FE, 0.15% P, AND 6-12% SIO2. |
|---|
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud |
| Rock unit name | Clay Residuum;Shady Dolomite |
| Rock description | Clay Residuum;Shady Dolomite |
| (1) | -78.51055, 38.56004 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Ne-Sw Trend |
| Type of structure | Local |
| Structure description | Syncline, Strike-Slip Fault |
| General form | IRREGULAR |
|---|---|
| Dip | NW |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1880 |
| Year of first production | 1895 |
| Year of last production | 1938 |
| District name | Elkton Area |
|---|
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | Paul Tyler |
| Year | 1920 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^39.77% Mn, Valued At ?14,474 | ||||||||||||||
| |||||||||||||||
| Year | 1929 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^38% Mn | ||||||||||||||
| |||||||||||||||
| Year | 1930 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Ap_Grade: ^41.5% Mn, 2.9% Fe, 16.8% Sio2: Valued At ?5,402 | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Year | 1931 | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | |||||||||||||||||||||
| Accuracy | Accurate | |||||||||||||||||||||
| Description | Ap_Grade: ^45% Mn, 2.8% Fe, Valued At ?6,074 | |||||||||||||||||||||
| ||||||||||||||||||||||
| Year | 1932 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ? | ||||||||||||||
| Description | Ap_Grade: ^42% Mn, Valued At $2,355 | ||||||||||||||
| |||||||||||||||
| Year | 1933 | |||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | |||||||||||||||||||||||||||||||||||
| Accuracy | Accurate | |||||||||||||||||||||||||||||||||||
| Description | Ap_Grade: ^43% Mn, 5% Fe, 13.4% Sio2, 0.12% P, Value- $14,186 | |||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
| Year | 1934 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||||||||||||||||
| Accuracy | Accurate | ||||||||||||||||||||||||||||
| Description | Ap_Grade: ^45.3% Mn, 8.7% Fe, 10% Sio2, Valued At ?3,572 | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Year | 1935 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^33% Mn, Valued At $909 | ||||||||||||||
| |||||||||||||||
| Year | 1935 | |||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | |||||||||||||||||||||||||||||||||||
| Accuracy | Accurate | |||||||||||||||||||||||||||||||||||
| Description | Ap_Grade: ^1210 Tons- Met., 45% Mn, 2.9% Fe, 0.45% P, 8.6% Sio2: 150 Tons- Misc., 42.5% Mn, 3% Fe, 9% Sio2, 0.12% P: Total Value $17,302. | |||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
| Year | 1936 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^50 Tons Metallurgical- 37% Mn, 350 Tons- 43.5% Mn, Totat Value $5,450 | ||||||||||||||
| |||||||||||||||
| Year | 1937 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^44% Mn, Valued At $1,568 | ||||||||||||||
| |||||||||||||||
| Year | 1938 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1920-1938 | ||||||||||||||
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^Metallurgical And Miscellaneous Ore, Averaged 41% Mn | ||||||||||||||
| |||||||||||||||
| Year | 1938 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^33.5% Mn, Valued At $450 | ||||||||||||||
| |||||||||||||||
| Year | 1938 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | ORE MN | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^43% Mn, Valued At $350 | ||||||||||||||
| |||||||||||||||
| Type of workings | Surface/Underground |
|---|---|
| Area | 1.619HA |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W000673 |
KING, P.B., 1950, GEOLOGY OF THE ELKTON AREA, VIRGINIA: USGS PROF. PAPER 230, 82 P.
KING, P.B., 1943, MANGANESE DEPOSITS OF THE ELKTON AREA, VIRGINIA: USGS BULL. 940-B, P. 15-55.
STOSE, G.W., MISER, H.D., KATZ, F.J., AND HEWETT, D.F., 1919, MANGANESE DEPOSITS OF THE WEST FOOT OF THE BLUE RIDGE, VIRGINIA: VA. GEOLOGICAL SURVEY BULL. 17, 166 P.
ALLEN, R.M., JR., 1967, GEOLOGY AND MINERAL RESOURCES OF PAGE COUNTY: VDMR BULL. 81, 78 P.
HARDER, E.C., 1910, MANGANESE DEPOSITS OF THE UNITED STATES: USGS BULL. 427, P. 55-56.
WATSON, T.L., 1907, MINERAL RESOURCES OF VIRGINIA: LYNCHBURG, VIRGINIA, J.P. BELL CO., 618 P.
MORRILL, P., 1972, VIRGINIA MINES AND MINERALS: ROCKS AND MINERALS MAGAZINE, VOL. 47, NO. 6, P. 370.
PRIME, F., JR., 1880, THE MINERAL RESOURCES OF THE PAGE VALLEY: THE VIRGINIAS, VOL. 1, P. 34-36.
REFERENCE(1)
UNPUBLISHED COBALT REPORT
| Subject category | Comment text |
|---|---|
| Deposit | MINE IS IN CLAYEY RESIDUUM OVERLYING THE LOWER BEDS OF THE SHADY DOLOMITE AND IS ON THE NORTHWARD PROJECTION OF A SYNCLINE WITH A STRIKE-SLIP FAULT OF RIGHT-LATERAL MOVEMENT LOCATED SOUTH OF THE MINE. JUST UPSLOPE THE CLAY IS BORDERED BY OUTCROPS OF THE ANTIETAM FORMATION. THE TWO LARGE OPENCUTS EXPOSE BUFF, BROWN, OR RED CLAY, IN PART SANDY, WITH A VARIED BUT OBSCURE DIP TO THE NORTHWEST. THE CLAY CONTAINS CHALCEDONIC CHERT, JASPEROID, MANGANESE NODULES AND VEINS OF LIMONITE. BETWEEN 1928-1937 NEAR THE WEST END OF THE NORTHERN OPENCUT, A LENS-SHAPED BODY OF SOLID MANGANESE ORE 3 M (10 FT) THICK, WHICH PINCHED OUT DOWN DIP, WAS MINED OUT. IN THE SOUTHERN OPENCUT A STEEP-SIDED DEPRESSION MAY BE SEEN IN THE CLAY THAT IS FILLED BY GRAVEL DEPOSITS CONSISTING OF RED SAND ENCLOSING DEEPLY WEATHERED SANDSTONE PEBBLES AND COBBLES. THIS MATERIAL CONTAINS MANY HIGHLY SILICEOUS, SPHERICAL AND BOTRYOIDAL MANGANESE NODULES WHICH WERE AVOIDED DURING MINING. BOTH THE RESIDUAL CLAYS AND THE ANCIENT |
| Deposit | GRAVELS ARE UNCONFORMABLY OVERLAIN BY FANGLOMERATES CONTEMPORANEOUS WITH THE OLDER GRAVEL UNIT, WHICH DIP STEEPLY AWAY FROM THE MOUNTAIN AND ATTAIN A THICKNESS OF 4.6 M (15 FT). THE FANGLOMERATE UNIT TRUNCATED VEINS OF LIMONITE AND MANGANESE IN THE CLAY, AND THE GRAVEL CONTAINS REWORKED MANGANESE FRAGMENTS DERIVED FROM THE CLAY. EXCEPT FOR THE SILICEOUS ORE IN THE GRAVEL DEPOSIT VERY LITTLE MANGANESE ORE IS PRESENT AND RESERVES ARE SMALL AT BEST. |
| Deposit | DURING THE TIME OF OPERATION THE SHENANDOAH VALLE Y MANGANESE CORP., THE MINE AND WASHER WERE CONNECTED WITH THE MAIN LINE OF THE NORFOLK AND WESTERN RAILROAD BY A BRANCH RAILWAY. THE WASHER WAS LOCATED ON THE EAST SIDE OF STONY RUN. DURING OPERATIONS BY TYLER THE ORE WAS HAULED FROM THE MINE BY TRUCK. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-AUG-1972 | Coury, Anny B. | U.S. Geological Survey | |
| Updater | 01-JUL-1982 | Trimble, David, C. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.