| Deposit ID | 10042521 |
|---|---|
| MRDS ID | M060338 |
| Record type | Site |
| Current site name | Bloody Canyon Mine |
| Alternate or previous names | Red Star, Hutton, Cosmopolitan |
| Related records | 10247673 |
| Geographic coordinates: | -118.13653, 40.51656 (WGS84) |
|---|---|
| Elevation | 1951 |
| Relative position | 10 MI. S OF IMLAY, NEVADA |
Political divisions (FIPS codes)
Pershing(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Star Peak(quadrangle 1:24,000 scale)
Eugene Mountains(quadrangle 1:100,000 scale)
Lovelock(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Dixie Valley(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 | Pershing |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 031N | 034E | 35 | Nevada |
| Commodity | Importance |
|---|---|
| Antimony Critical | Primary |
| Silver | Primary |
| Iron | Tertiary |
| Lead | Tertiary |
| Materials | Type of material |
|---|---|
| Stibnite | Ore |
| Quartz | Gangue |
| Chalcopyrite | Unknown |
| Pyrite | Unknown |
| Model code | 273 |
|---|---|
| USGS model code | 36a |
| Deposit model name | Low-sulfide Au-quartz vein |
| Mark3 model number | 27 |
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||
| Rock unit name | Rochester Rhyolite;Star Peak Formation;Star Peak Formation;Star Peak Formation | ||
| Rock description | Rochester Rhyolite;Star Peak Formation;Star Peak Formation;Star Peak Formation | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| Rock unit name | Koipato Group; |
| Rock description | Koipato Group; |
| (1) | Humboldt Assemblage - Limestone, dolomite, shale, sandstone, and conglomerate |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Reg.Struct: Faults And Cross Faults, Tnding N-S, Nne-Ssw, Cause Alot Of Gouge |
| Type of structure | Local |
| Structure description | Faults And Cross-Faults Trending N-S, Nne-Ssw |
| General form | VEINS |
|---|---|
| Thickness | 3.66M |
| Depth to top | 0M |
| Depth to bottom | 60.96M |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1868 |
| Year of first production | 1871 |
| District name | Star District |
|---|
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | Neal, Hybert L. |
| Home office | Winnemucca, Nev. |
| First year | 1960 |
| Year | 1907 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | SB ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^60 % Sb | ||||||||||||||
| |||||||||||||||
| Year | 1912 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | SB ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^60 % Sb | ||||||||||||||
| |||||||||||||||
| Year | 1938 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | SB ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^60 % Sb | ||||||||||||||
| |||||||||||||||
| Year | 1940 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | SB ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^13% Sb | ||||||||||||||
| |||||||||||||||
| Year | 1942 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Material | SB ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Ap_Grade: ^55% Sb | ||||||||||||||
| |||||||||||||||
| Year | 1942 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | To 1942 | ||||||||||||||
| Material | ORE SB AG | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^60 % Sb | ||||||||||||||
| |||||||||||||||
| Type of workings | Surface/Underground |
|---|---|
| Length | 91.44M |
| Overall depth | 60.96M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M060338 |
JOHNSON, M.G., 1977, GEOLOGY AND MINERAL DEPOSITS OF PERSHING COUNTY, NEVADA; NBMG BULL. 89
LAWRENCE, 1963, ANTIMONY DEPOSITS OF NEVADA; NBMG BULL. 61
RAYMOND, 1873, STATISTICS OF MINES AND MINING IN THE STATES AND TERRITORIES WEST OF THEOCKY MOUNTAINS, 5TH MANAUL REPORT; WASHINGTON, GOVT. PRINTING OFFICE
LAWRENCE, 1963
| Subject category | Comment text |
|---|---|
| Deposit | DEPOSIT CONSISTS OF AN EAST AND WEST VEIN. THE ORE WAS MOSTLY HIGH QUALITY ANTIMONY ASSOCIATED WITH AG AND MINOR PB, CONTAINED IN 2 QUARTZ STIBNITE VEINS A FEW FEET THICK ABOUT 200 FEET APART IN A MINERALIZED ZONE OF STEEPLY DIPPING FISSURE VEINS. THE WEST VEIN IS OFFSET BY AN EAST-WEST FAULT WITH THE NORTHERN SEGMENT STRIKING N10E AND DIPS 85 DEGREES W AND IS RELATIVELY BARREN; THE SOUTHERN SEGMENT STRIKES N10W, DIPS 80-85 DEGREES E AND CONTAINS ABUNDANT STIBNITE. THE EAST VEIN STRIKES N10-25E AND DIPS 80-85E AND INTERSECTS A BARREN FAULT WITH STRIKE N25E, DIPPING EAST. STIBNITE OCCURS AS PODS, STREAKS AND SINGLE CRYSTALS IN THE QUARTZ, AND IN GOUGE. PYRITE IS COMON BOTH IN VEINS AND DISSEMINATED THROUGH WALL ROCK. LIMESTONNE, SANDSTONE AND SILTSTONES OF THE STAR PEAK FORMATION OVERLIE THE RHYOLITE AND CROP OUT A SHORT DISTANCE WEST OF THE WORKINGS. ORE IS CONFINED TO RHYOLITE.; MODEL NAME COULD ALSO BE: SIMPLE SB. |
| Deposit | DISCOVERED IN 1868. ANTIMONY FIRST PRODUCED IN 1871.OTHER YEARS OF PRODUCTION 1907, 1912, 1917-21, 1938, 1940, 1942. MINE WORKED INTERMITTENTLY TO 1942. THIS MINE WAS ONE OF THE LARGEST PRODUCERS OF ANTIMONY ORE IN NEVADA. MOST OF ORE WAS MINED FROM THE SOUTH SEGMENT OF THE WEST VEIN BY STOPING FROM THE MAIN ADIT THAT CUTS THE VEIN 200 FEET BELOW SURFACE. SEVERAL SHORT ADITS AND TRENCHES EXPLORE SURFACE EXPOSURES OF WESTVEIN AND ALSO FOLLOW THE EAST VEIN. ; INFO.SRC : 1 PUB LIT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1979 | Donahoe, James L. (Johnson, M.G.) | Nevada Bureau of Mines and Geology | |
| Updater | 01-JAN-1981 | Royse, Sue E. | Nevada Bureau of Mines and Geology | |
| Updater | 01-SEP-1994 | Li, Zhiping (Peters, S.) | U.S. Geological Survey |
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.