| Deposit ID | 10310427 |
|---|---|
| Record type | Site |
| Current site name | Gunman Property |
| Alternate or previous names | RH Zone, RH South Zone |
| Geographic coordinates: | -115.753, 39.87241 (WGS84) |
|---|---|
| Elevation | 2010 |
| Relative position | The property is located about 40 miles NNE of Eureka on the east side of the Diamond Mountains. PS: Reporter entered lat/long degrees only (no minutes or seconds) and UTM coordinates. Also, the 39 lat was in the longitude field and the 115 long was in the latitude field. I used http://www.uwgb.edu/dutchs/UsefulData/UTMConversions1.xls to convert UTM to lat/long. |
Political divisions (FIPS codes)
White Pine(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Christina Peak(quadrangle 1:24,000 scale)
Newark Lake(quadrangle 1:100,000 scale)
Ely(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Little Smoky-Newark Valleys(hydrologic unit)
Central Nevada Desert Basins(hydrologic accounting unit)
Central Nevada Desert Basins(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 | White Pine |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 023N | 055E | 14 | Nevada |
| Commodity | Importance |
|---|---|
| Zinc Critical | Primary |
| Silver | Primary |
| Materials | Type of material |
|---|---|
| Smithsonite | Ore |
| Calcite | Gangue |
| Model code | 72 |
|---|---|
| USGS model code | 19a |
| Deposit model name | Polymetallic replacement |
| Mark3 model number | 47 |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||
| Rock type qualifier | carbonaceous | ||
| Rock unit name | Carbon Ridge Formation | ||
| |||
| (1) | -115.753, 39.87241 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | The regionally extensive, north-trending Phillipsburg fault is a Cenozoic normal fault that dips about 45 degrees west and extends for at least 40 km along the west flank of the Diamond Mountains. |
| Type of structure | Local |
| Structure description | Proximity to strong north trending faults appears to be a controlling factor on grade distribution. |
| General form | tabular to blanket |
|---|
| Operation type | Surface |
|---|---|
| Development status | Prospect |
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | Yes |
| Discovery year | 2000 |
| District name | Diamond Range (no district) |
|---|
| Ownership category | BLM Administrative Area |
|---|---|
| Area name | Ely BLM District |
| Type | Owner |
|---|---|
| Owner | Cypress Development Corp. in the 2,400 acres Gunman Zinc-Silver Project |
| Interest | 73.13 |
| Year | 2006 |
| Type | Owner |
|---|---|
| Owner | Bison Gold Exploration Inc. in the 2,400 acres Gunman Zinc-Silver Project (2006) |
| Interest | 26.87 |
| Year | 2006 |
| Type | Operator |
|---|---|
| Owner | Cypress Development Corp. |
| Year | 2004 |
NBMG MI-2002
Cypress Development Corp. website and press releases 2000-2004
| Subject category | Comment text |
|---|---|
| Deposit | The mineralization is shallow occurring mainly between the surface and 300 foot depth and consists of a high-grade zinc oxide zone surrounded by a zinc-bearing carbonate replacement envelope. The RH Zone is a tabular body of intensely oxidized, zinc-silver mineralization of apparent carbonate replacement origin. The zinc mineralization is primarily zinc oxide (smithsonite). As partially delineated by the 2000 drill program, the RH Zone is approx. 300 feet long (NNW), 150 feet wide (ENE), and about 80 feet thick starting at or near surface and continues to be open along strike in both directions. Drilling has indicated that mineralization occurs in vertical bodies within a flat lying oxidized zone up to 300 feet thick extending down from the surface. The immediate drill target now covers an area at least 2000 feet long by 500 feet wide. Drilling within this envelope is currently targeting features identified during a Self Potential (SP) survey carried out in 2001 that showed very distinct signatures over the high-grade RH Zone and the RH South Zone. The SP survey showed classic responses from the upper oxidized zone and over sulfides in the lower reduced part of the section. Proximity to strong north trending faults appears to be a controlling factor on grade distribution. The mineralization discovered on the Gunman Project to date, strongly resembles the oxide zinc-silver-lead-gold bonanzas that have been historically mined in the Eureka district, located 40 miles SSW of the Gunman property. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-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.