| Deposit ID | 10310362 |
|---|---|
| MRDS ID | M231715 |
| Record type | Site |
| Current site name | Northumberland Mine |
| Alternate or previous names | Blue Bell, Monitor, Last Chance Group, Cyprus-Northumberland Mine |
| Related records | 10106925 |
| Geographic coordinates: | -116.84675, 38.95826 (WGS84) |
|---|---|
| Elevation | 2710 |
| Relative position | The Northumberland Mine is located about 65 miles north-northeast of Tonopah. |
Political divisions (FIPS codes)
Nye(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Northumberland Pass(quadrangle 1:24,000 scale)
Mount Jefferson(quadrangle 1:100,000 scale)
Tonopah(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Diamond-Monitor Valleys(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 | Nye |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 013N | 045E | 24 | Nevada | |
| Mount Diablo | 013N | 046 E | 19 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Barium-Barite Critical | Secondary |
| Arsenic Critical | Tertiary |
| Iron | Tertiary |
| Materials | Type of material |
|---|---|
| Pyrargyrite | Ore |
| Cerargyrite | Ore |
| Arsenopyrite | Ore |
| Gold | Ore |
| Scorodite | Ore |
| Quartz | Ore |
| Sericite | Ore |
| Barite | Ore |
| Model code | 173 |
|---|---|
| USGS model code | 26a.1 |
| Deposit model name | Sediment-hosted Au |
| Mark3 model number | 17 |
| Model code | 172 |
| USGS model code | 26a |
| Deposit model name | Carbonate-hosted Au-Ag |
| Mark3 model number | 15 |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale | ||||
| Rock type qualifier | carbonaceous | ||||
| Rock unit name | Pogonip Group | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale | ||||
| Rock type qualifier | calcareous | ||||
| Rock unit name | Pogonip Group | ||||
| |||||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Metamorphic Rock > Metasedimentary Rock > Quartzite | ||
| Rock unit name | Vinini Fm | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Chemical Sediment > Chert | ||
| Rock unit name | Vinini Fm | ||
| |||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Argillite | ||||
| Rock unit name | Roberts Mountain Fm | ||||
| |||||
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||||
| Rock unit name | Roberts Mountain Fm | ||||
| |||||
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Granitoid > Quartz Monzonite | ||||
| |||||
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Porphyry | ||
| Rock type qualifier | quartz-eye | ||
| |||
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | |||||
| Rock unit name | Northumberland intrusive | ||||
| |||||
| (1) | -116.84675, 38.95826 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Major thrust sheets have affected the rocks. A Jurassic granodioritic stock has domed the country rocks. |
| Type of structure | Local |
| Structure description | Silicified horizons of the Pogonip group rocks have been extensively fractured and microfractured. |
| General form | tabular to irregular |
|---|
| Operation type | Surface-Underground |
|---|---|
| Development status | Producer |
| Commodity type | Both |
| Deposit size | Medium |
| Significant | Yes |
| Discovery year | 1866 |
| Discoverer | A prospector named Logan |
| Year of first production | 1860 |
| Year of last production | 1988 |
| Production years | 1860s-1891\n1939-1942\n1981-1988\n |
| District name | Northumberland District |
|---|
| Ownership category | National Forest |
|---|---|
| Area name | Tonopah USFS Administrative District |
| Type | Owner |
|---|---|
| Owner | NewWest Resources Group's Nevada Western Gold Corporation |
| Year | 2005 |
| Type | Operator |
|---|---|
| Owner | Newmont Mining Corporation |
| Year | 2005 |
Kleinhampl, F.J. and Ziony, J.I., 1984, NBMG Bull 99-A and B.
Kral, V. E., 1950, NBMG Bull 50.
Unpublished notes, Nbmg mining district file 42, Item 2.
Nevada Mining Association Newsletter, Oct., 1980.
Field examination of the property, and discussion, L.J. Garside and H.F. Bonham, Jr.,NBMG, May, July, 1981.
Smith, P. and Bentz, J., 1981, NBMG Field Examination.
Tingley, J.V. and Quade, Jack, 1986, NBMG OFR 86-14.
Goldstein, I.J., 1973, Gold Mineralization at the Northumberland Gold Mine, Nye Co., NV; GSA Abstr. Poster session
McKee, E.H., 1974, NBMG Report 19
Motter, J.W. and Chapman, P.E., 1984, AEG Field Trip Guidebook.
Ott, L.E., 1983, Geol. and Mineralization at Northumberland Gold Mine, Nye Co. Nv; MS Thesis; Montana College of Mineral Science and Technology.
NBMG MI-1987
NBMG Mining District File 242, news Clippings.
NBMG, MI-79 thru MI-84, MI-86 thru MI-03
NBMG Map 91, 1st, 2nd, 3rd.
Amer. Mines (1989), 1989 thru Amer. Mines (2001), 2000
websites - Newmont and NewWest Resources Group.
| Subject category | Comment text |
|---|---|
| Deposit | There are 3 main veins at the deposit: Lady Cummings, Northumberland, and Detroit veins. Disseminated gold mineralization occurs largely in a carbonaceous shale bed near contact of granitic intrusive. Ore is present in both upper and lower plate rocks along thrust fault. Siltstone and limestone have been considerably replaced by jasperoid, which is locally hydrothermally brecciated. Late-stage veinlets contain coarse barite crystals. Ore is strongly altered, iron-oxide-stained, thin-bedded carbonaceous shale. On the west side of the canyon are highly altered, fractured volcanic rocks. Gold occurs in microfracture fillings of quartz and barite in silicified horizons of the Ordovician Pogonip Group associated with the margins of a monzonite intrusive. Disseminated gold mineralization occurs largely in a carbonaceous shale bed near the contact with a granitic intrusive. Ore is present in both upper and lower plate rocks along a thrust fault. Siltstone and limestone have been considerably replaced by jasperoid, which is locally hydrothermally brecciated. Late stage veinlets contain coarse barite crystals. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-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.
MRDS records operators as of each record's last update (≤ 2019). Some of the operators listed here have since changed hands or dissolved:
Curated by qvyshift.com from publicly-reported M&A activity (SEC filings, press releases, USGS Mineral Yearbooks). Not authoritative — verify against primary sources before relying on it. The MSHA panel above is the current authoritative source for actively-permitted mines.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.