| Deposit ID | 10310315 |
|---|---|
| MRDS ID | M232855 |
| Record type | Site |
| Current site name | Victorine Gold Mine |
| Alternate or previous names | Victorine Gold Project, Sumich Deposit, Bimetallic Mine, Phoenician, Kingston Mine, Klondike Mine |
| Related records | 10045171, 10045172, 10047157 |
| Geographic coordinates: | -117.13537, 39.22714 (WGS84) |
|---|---|
| Elevation | 2410 |
| Relative position | The Victorine Mine is located about 20 miles south of Austin in Kingston Canyon on the eastern flank of the Toiyabe Range. |
Political divisions (FIPS codes)
Lander(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Brewer Canyon(quadrangle 1:24,000 scale)
Smith Creek Valley(quadrangle 1:100,000 scale)
Millett(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Northern Big Smoky Valley(hydrologic unit)
Central Nevada Desert Basins(hydrologic accounting unit)
Central Nevada Desert Basins(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
Humboldt-Toiyabe National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Nevada | Lander |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 016N | 043E | 27 22 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Copper | Secondary |
| Lead | Tertiary |
| Zinc Critical | Tertiary |
| Antimony Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Silver | Ore |
| Argentite | Ore |
| Tetrahedrite | Ore |
| Chalcopyrite | Ore |
| Galena | Gangue |
| Sphalerite | Gangue |
| Pyrite | Gangue |
| Model code | 85 |
|---|---|
| USGS model code | 22c |
| Deposit model name | Polymetallic veins |
| Mark3 model number | 46 |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||||
| Rock unit name | Broad Canyon sequence | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Siltstone | ||||
| Rock type qualifier | calcareous | ||||
| Rock unit name | Broad Canyon sequence | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Argillite | ||||
| Rock type qualifier | calcareous | ||||
| Rock unit name | Broad Canyon sequence | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Metamorphic Rock > Phyllite | ||||
| Rock type qualifier | graphitic | ||||
| Rock unit name | Broad Canyon sequence | ||||
| |||||
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite | ||
| Rock type qualifier | sills | ||
| |||
| (1) | -117.13537, 39.22714 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | The Kingston Canyon Thrust Fault is exposed just south of the mine area. |
| Type of structure | Regional |
| Structure description | Roberts Mountains Thrust Fault |
| General form | tabular |
|---|
| Operation type | Surface-Underground |
|---|---|
| Development status | Producer |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Discovery year | 1862 |
| Year of first production | 1865 |
| Year of last production | 1989 |
| Production years | 1865-71;1937-41; 1986-1989 |
| District name | Kingston District |
|---|
| Ownership category | Private |
|---|---|
| Ownership category | National Forest |
| Area name | Tonopah Forest Service Administrative District |
| Type | Owner-Operator |
|---|---|
| Owner | Goldrea Resources Corp. |
| Interest | 50 |
| Year | 2004 |
| Type | Owner-Operator |
|---|---|
| Owner | Stirrup Creek Gold, Ltd. |
| Interest | 50 |
| Year | 2004 |
Stewart, J.H., McKee, E.H., and Stager, H.K., 1977, Geology and Mineral Deposits of Lander County Nevada: NBMG Bull. 88.
Sizer, F.L., 1893, Report on the Kingston Group of Mines (Unpub): NBMG Mining District Files
Brown, A.H., 1909, Unpublished report on the Kingston Property: NBMG Mining District Files
Tingley, J. V., 1981, Field Examination Report, Sept 21, 1981.
Unpublished reports to stockholders, 1983, New Beginnings Resources, Inc.
NBMG Map 84, 1983, Active Mines and Oil Fields
State Division of Mine Inspection, 1983, Directory of Nevada Mine Operations active during calendar year 1983.
NBMG, 1994, MI-1993
New genetic and structural interpretation of the quartz-gold deposits in the Kingston District, Nevada; 1998, North American Conference on Tectonic Control of Ore Deposits and the Vertical and Horizontal Extent of Ore Systems : proceedings volume / editors, Geza Kisvarsanyi, Sheldon K. Grant.: University of Missouri-Rolla, Rolla, Mo., p. 103-108.
Kuehn, Carl A., 1984, Geology and exploration geochemistry of the Big Creek and Kingston Canyon areas, Toiyabe Range, Lander County, Nevada; M.S. Thesis, Pennsylvania State University, 1984, 217 p.
Akright, Robert L., 1990, Geology of the Sumich (Victorine) Deposit, Kingston District, Lander County, Nevada. in Discoveries of valuable minerals and precious metals deposits related to intrusions and faults; Case histories of mineral discoveries; Volume 2, p. 353-357, Victor F. Hollister, editor, Littleton, Colo. : Society for Mining, Metallurgy, and Exploration, 1990.
Northern Miner, 1/15/96.
| Subject category | Comment text |
|---|---|
| Deposit | The Victorine Mine deposit consists of a shallowly-dipping gold-and silver-bearing quartz vein system. The ore occurs as pockets and veinlike masses of quartz along a silicified zone in limestone at the top of a lower Cambrian map unit. The ore zone trends east and in general, dips 20-30 degrees north, conformable to the host rocks. The vein forms a prominent outcrop, 3 to 8 feet thick, which is traceable for more than a mile along strike. The vein system includes a main (lower) vein about 28 fet thick and several smaller veins lying above the main vein. Drill- and surface observations indicate that the main vein follows a thrust fault. Renewed movement along the thrust brecciated the vein material and provided pathways for repeated subsequent vein emplacement. Up to 5 episodes of brecciation and vein emplacement are documented with the richest gold deposition event being one of the later events. The ore-controlling thrust lies below the Roberts Mountains thrust fault and cuts a series of graphitic shales interbedded with limestones. The host rocks along the vein exhibit intense drag-folding. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-SEP-2005 | LaPointe, D.D. | Nevada Bureau of Mines and Geology | |
| Editor | 01-SEP-2007 | Schruben, Paul G. | U.S. Geological Survey | Converted from S&A FileMaker format to Oracle. Edit checks on rocks, units, and ages with Geolex search, and other fields. |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.