| Deposit ID | 10310419 |
|---|---|
| MRDS ID | W002900 |
| Record type | Site |
| Current site name | Gemfield Gold Deposit |
| Related records | 10310328, 10310417, 10310418, 60001656 |
| Geographic coordinates: | -117.23341, 37.71023 (WGS84) |
|---|---|
| Elevation | 1830 |
| Relative position | The deposit is located about two miles north of the historic mining town of Goldfield about 28 miles south of Tonopah, near the east border of Esmeralda County |
Political divisions (FIPS codes)
Esmeralda(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Goldfield(quadrangle 1:24,000 scale)
Goldfield(quadrangle 1:100,000 scale)
Goldfield(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Ralston-Stone Cabin Valleys(hydrologic unit)
Central Nevada Desert Basins(hydrologic accounting unit)
Central Nevada Desert Basins(hydrologic subregion)
Great Basin(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Nevada | Esmeralda |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 002S | 042E | 27 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Secondary |
| Copper | Secondary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Quartz | Gangue |
| Alunite | Gangue |
| Barite | Gangue |
| Gypsum | Gangue |
| Limonite | Gangue |
| Kaolin | Gangue |
| Model code | 154 |
|---|---|
| USGS model code | 25e |
| Deposit model name | Epithermal quartz-alunite Au |
| Mark3 model number | 38 |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||
| Rock unit name | Sandstorm Rhyolite | ||
| |||
| (1) | -117.23341, 37.71023 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | The Gemfield Deposit is located to the west of the ring fracture zone that controls the main Goldfield deposits. |
| Type of structure | Regional |
| Structure description | Tertiary deposits are domed and faulted by steeply dipping post Miocene: N-S and E-W faults. |
| General form | Irregular to tabular or knobby |
|---|
| Operation type | Surface-Underground |
|---|---|
| Development status | Producer |
| Commodity type | Metallic |
| Deposit size | Medium |
| Significant | Yes |
| Discovery year | 1902 |
| Year of first production | 1904 |
| Year of last production | 1970 |
| Production years | 1904-1970s |
| District name | Goldfield District: |
|---|
| Ownership category | Private |
|---|---|
| Ownership category | BLM Administrative Area |
| Area name | Tonopah District BLM |
| Type | Owner-Operator |
|---|---|
| Owner | Metallic Ventures Inc. |
| Year | 2004 |
Ransome, F. L. 1909, Geol. and Ore Deposits of Goldfield, Nev.: USGS Prof. Paper 66, 258 p.
Searls, F. Jr., 1948, Geol and Ore Deposits of Goldfield, Nev.: Nevada Univ. Bull., v.42, no. 5, Geology and Mining Ser. 48, 24 p.
Spurr, J E, 1905, The Ores of Goldfield, Nev.: USGS Bull. No. 260, p. 132-139.
Lincoln, F C, 1923, Mining Dist and Min. Res. Nev.: Reno, Nev. Newsletter Pub., p. 67-73
Albers, J.P. and Stewart, J.H., 1972, Geology and Mineral Deposits of Esmeralda County, Nevada: NBMG Bull. 78, p. 67-69
Steven Ristorcelli, Scott Hardy, and Neil Prenn, 2003, Geology and Mineralization of the Goldfield Area, Esmeralda,County, Nevada; Geological Society of Nevada Special Publication No. 37: Spring 2003 Field Trip Guidebook Gold Deposits of the Goldfield, Midway and Thunder Mountain Areas
Internet website for Metallic Ventures Inc.
NBMG MI-80 through MI-99
NBMG Map 91 1st, 2nd, 3rd
MAS, 1984
Amer. Mines (1990-2001)
NBMG Bull 78
Metallic Ventures Inc., press releases 12/23/02.
Metallic Ventures Gold Inc. Press Release: July 25, 2006
| Subject category | Comment text |
|---|---|
| Deposit | The drill-defined parts of the Gemfield mineralized area has the following dimensions: 2,500 ft long, 2,000 ft down dip, and an average 150 ft thick. Almost all of the precious and base metal production recorded from the Goldfield mining district has come from rich epithermal bonanza ore bodies in the area northeast of the Goldfield town site. These ore bodies occur within silicified hydrothermal alteration zones. Mineralization in the argillized wall rock envelopes appears to be leakage zones emanating from core silicified zones. Ore zones are commonly associated with silicification and/or free quartz surrounded by large envelopes of intense argillic alteration. In the main district, gold-copper ores were found in a series of pipe-like shoots referred to locally as ledges, the most productive of which occurred where the east-west striking Goldfield structural trend intersects a mile-long arcuate section of inferred intrusive-related ring-fracture zone. Although the major ore bodies are hosted in a complex intersecting set of faults and fracture zones, the ore-bearing structures are generally north-south trending and sub-parallel to the strike of the ring-fracture zone in that location. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAY-2004 | 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.