| Deposit ID | 10080108 |
|---|---|
| MRDS ID | W031185 |
| Record type | Site |
| Current site name | White Peak No. 1 Mine |
| Alternate or previous names | Purcell Mines, Miller Mines |
| Geographic coordinates: | -77.78999, 37.5445 (WGS84) |
|---|---|
| Elevation | 114 |
| Relative position | MINE IS 2.3 MILES NORTHEAST OF FLAT ROCK. |
Political divisions (FIPS codes)
Powhatan(county)
Virginia(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Fine Creek Mills(quadrangle 1:24,000 scale)
Richmond(quadrangle 1:100,000 scale)
Richmond(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Middle James-Willis(hydrologic unit)
James(hydrologic accounting unit)
Lower Chesapeake(hydrologic subregion)
Mid Atlantic(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Virginia | Powhatan |
| Commodity | Importance |
|---|---|
| Mica | Primary |
| Tantalum Critical | Secondary |
| Niobium (Columbium) Critical | Secondary |
| Materials | Type of material |
|---|---|
| Muscovite | Ore |
| Biotite | Gangue |
| Plagioclase | Gangue |
| Quartz | Gangue |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Gneiss |
| Rock unit name | Chopawamsic Formation |
| Rock description | Chopawamsic Formation |
| (1) | -77.78999, 37.5445 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Ne-Sw Trend |
| Type of structure | Local |
| Structure description | Faults |
| General form | LENS |
|---|---|
| Strike | N 85 DEG E |
| Dip | NEARLY VERTICAL |
| Plunge direction | WESTWARD |
| Length | 69M |
| Width | 11M |
| Depth to top | 0M |
| Depth to bottom | 14M |
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1895 |
| Discoverer | Mr. Wells And Mr. Miller |
| Year of first production | 1895 |
| District name | Powhatan Area |
|---|
| Ownership category | Private |
|---|
| Type | Operator |
|---|---|
| Owner | Jacob Van Doren |
| Type | Owner |
|---|---|
| Owner | James M. Purcell |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W031185 |
BROWN, W.R., 1962, MICA AND FELDSPAR DEPOSITS OF VIRGINIA: VIRGINIA DIVISION OF MINERAL RESOURCES, MINERAL RESOURCES REPORT 3, 195 P.
DIETRICH, R.V., 1970, MINERALS OF VIRGINIA: VIRGINIA POLYTECHNIC INSTITUTE, RESEARCH DIVISION BULLETIN 47, WILLIAMS PRINTING CO., RICHMOND, VA., 325 P.
MITCHELL, R.S., 1965, VIRGINIA METAMICT MINERALS: COMMENTS ON A URANIUM-NIOBIUM OXIDE FROM POWHATAN COUNTY, SOUTHEASTERN GEOLOGY, VOL. 6, NO. 2, PP. 79-85.
1895 DIREXPL WELLS AND MILLER-OPENED MINE
1905 DIREXPL MR. STRATER-OPERATED MINE
1942 DIREXPL W.W. HOWE-EXPLORATION OF SITE
1944 DIREXPL JACOB VAN DOREN-CONTINUED EXPANSION, MINED
1944 DIREXPL VIRGINIA MANGANESE CORP. - EXPANDED WORKINGS, MINED
BROWN (1962)
| Subject category | Comment text |
|---|---|
| Deposit | THE MAIN BODY OF THE PEGMATITE IS DISCORDANT TO THE FOLIATION OF THE COUNTRY ROCK, ALTHOUGH NUMEROUS STRINGERS AND OFFSHOOTS PENETRATE ALONG THE FOLIA. THE PEGMATITE HAS A QUARTZ CORE UP TO 3.7 M (12 FT) THICK, THAT EXTENDS THROUGHOUT THE LENGTH OF THE DIKE. SOME PERTHITE AND BIOTITE OCCUR WITHIN THE QUARTZ. THE CORE IS SURROUNDED BY A WALL-ZONE AGGREGATE OF KAOLINIZED PLAGIOCLASE, INTERSTITIAL QUARTZ, AND LARGE MICA BOOKS. THE PLAGIOCLASE COARSENS INWARD FROM THE WALLS AND BECOMES VERY COARSE GRAINED ALONG THE CORE. SOME FRIABLE PERTHITE OCCURS WITHIN THE WALL ZONE. THE THIN BORDER ZONE CONSISTS OF FINE-GRAINED PLAGIOCLASE AND QUARTZ. MICA HAS BEEN RECOVERED CHIEFLY FROM THE OUTER PART OF THE WALL ZONES. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1981 | Trimble, David C. (Sweet, Palmer C.) | Virginia Division of Mineral Resources | |
| Updater | 01-DEC-1987 | Sweet, Palmer C. | Virginia Division of Mineral Resources |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.