| Deposit ID | 10310558 |
|---|---|
| Record type | Site |
| Current site name | Pamlico Gold Property |
| Related records | 10037453 |
| Geographic coordinates: | -118.47289, 38.45548 (WGS84) |
|---|---|
| Elevation | 1680 |
| Relative position | The Pamlico Mining District is located on the south flank of the Garfield Hills, approximately 10 miles SE of Hawthorne.\n |
Political divisions (FIPS codes)
Mineral(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Pamlico(quadrangle 1:24,000 scale)
Excelsior Mountains(quadrangle 1:100,000 scale)
Walker Lake(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Walker Lake(hydrologic unit)
Walker(hydrologic accounting unit)
Central Lahontan(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management NV)
Bureau of Land Management NV BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Nevada | Mineral |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 007N | 031E | 13 14 23 24 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Secondary |
| Lead | Secondary |
| Zinc Critical | Secondary |
| Arsenic Critical | Tertiary |
| Manganese Critical | Tertiary |
| Materials | Type of material |
|---|---|
| Gold | Ore |
| Galena | Ore |
| Quartz | Gangue |
| Limonite | Gangue |
| Pyrite | Gangue |
| Model code | 273 |
|---|---|
| USGS model code | 36a |
| Deposit model name | Low-sulfide Au-quartz vein |
| Mark3 model number | 27 |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite | ||
| Rock type qualifier | tuff | ||
| Rock unit name | Excelsior Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff | ||
| Rock type qualifier | latite | ||
| Rock unit name | Excelsior Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Volcanic Breccia (Agglomerate) | ||
| Rock type qualifier | latite agglomerate | ||
| Rock unit name | Excelsior Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||
| Rock unit name | Excelsior Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||
| Rock type qualifier | laminated tuff | ||
| Rock unit name | Excelsior Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff | ||
| Rock type qualifier | laminated rhyolite | ||
| Rock unit name | Excelsior Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | |||
| Rock unit name | Gold Range Formation | ||
| |||
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Metamorphic Rock > Metavolcanic Rock | ||
| Rock unit name | Dunlap Formation | ||
| |||
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | |||||
| Rock unit name | quartz monzonite | ||||
| |||||
| (1) | -118.47289, 38.45548 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | The Luning-Fencemaker Thrust Belt lies directly east of the Sierra Nevada batholith and comprises a 500- kilometer long, 100 kilometer wide belt of intensely folded and thrusted Triassic and Jurassic marine sedimentary rocks. Individual thrust systems of note include the Luning, Fencemaker, Pamlico, Boyer, and Wild Horse thrusts (Speed and others, 1988). Thrusts of the LFTB generally carried deep-water, fine-grained turbiditic facies eastward and juxtaposed them against shallow-marine facies of the same age. |
| Type of structure | Local |
| Structure description | The Pamlico Anticline trends NW, derived on basis of relation between latite tuff and agglomerate unit with overlying rhyolitic tuff; this contact forms main localizing structure for Pamlico veins. |
| General form | irregular lenses |
|---|
| Operation type | Surface-Underground |
|---|---|
| Development status | Past Producer |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Discovery year | 1885 |
| Year of first production | 1886 |
| District name | Pamlico (Ashby, Oro, Hawthorne ) District |
|---|
| Ownership category | Private |
|---|---|
| Ownership category | BLM Administrative Area |
| Area name | Walker Resource area of the Carson City BLM administrative district |
| Type | Owner-Operator |
|---|---|
| Owner | American Bonanza Gold Mining Corp. |
| Year | 2004 |
Hill, J. M., 1915 , Some mining districts in NE Calif. and NW Nevada, USGS, Bull. 594
Vanderburg, 1937, Reconnaissance of Mining Districts n Mineral Co., Nev., USBM, Information Circular.
Ross, D. L., 1961 , Geology and Mineral Deposits of Mineral Co., Nev., NBMG Bull. 58
Archbold and Paul, 1970,Geology and mineral deposits of the Pamlico mining district, Mineral County, Nevada, NBMG Bull. 74.
Tingley, Joseph V., 1990, MINERAL RESOURCE INVENTORY BUREAU OF LAND MANAGEMENT, CARSON CITY DISTRICT, NEVADA, NBMG OPEN-FILE REPORT 90-1, p170-173.
Northern Miner, 12/26/94, 2/27/95, 4/10/95, 6/14/99
BLM Files, Carson City District
McArthur, Gerald F., October 9, 2002, SUMMARY GEOLOGICAL REPORT FOR THE GOLD BAR PROPERTIES, EUREKA COUNTY AND THE PAMLICO PROPERTY, MINERAL COUNTY NEVADA, U.S.A. SEC Disclosure form.
American Bonanza Gold Mining Corp., 2/24/03
The records of the historic Pamlico Mining Company are archived in the Special Collections of the University of Nevada, Reno library. They are contained in one Hollinger archival document case and cover the time period from 1888 through 1904. The material consists mainly of correspondence and financial statements and accounts. Most of the material is original and handwritten.
| Subject category | Comment text |
|---|---|
| Deposit | Workings have been developed along four main veins. Vein A strikes N65W and dips 27-55 SW; vein B strikes N55-70W and dips 25-70NE; vein P strikes N30-80W and dips 25-60NE; and a trough-shaped P-branch vein plunges 30SE with both flanks dipping 30 degrees towards the axis of the trough. Some ore forms irregular replacement bodies consisting of siliceous, ferruginous, locally jasperoidal, gossan material occupying a fracture zone. Vein filling is predominantly quartz, most commonly massive with substantial amounts of limonite and rare grains of pyrite. Small amounts of secondary copper minerals rarely coat fractures in veins. Gold reportedly formed wires and nuggets in the veins and was associated with pyritic portions of veins. Gold values in veins are erratic; reportedly some veins were followed for 300 ft. without finding any ore. Most veins now exposed underground are barren. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-2006 | 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.