| Deposit ID | 10037294 |
|---|---|
| MRDS ID | M031259 |
| Record type | Site |
| Current site name | Lexington Mine |
| Alternate or previous names | Lexington Tungsten Mine, Lexington Canyon Mine, Bonanza Mine, Bonanzy Claims Or Mine, Usbm Sample Locality #28. |
| Geographic coordinates: | -114.21251, 38.85134 (WGS84) |
|---|---|
| Elevation | 2676 |
| Relative position | NEAR HEAD OF LEXINGTON CREEK. THE LEXINGTON DISTRICT IS SOUTH OF SNAKE CREEK ON THE EAST SIDE OF THE SNAKE RANGE, ABOUT 5 TO 10 MILES SOUTHWEST OF GARRISON, UTAH. |
Political divisions (FIPS codes)
White Pine(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Arch Canyon(quadrangle 1:24,000 scale)
Garrison(quadrangle 1:100,000 scale)
Lund(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Hamlin-Snake Valleys(hydrologic unit)
Great Salt Lake(hydrologic accounting unit)
Great Salt Lake(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 | 11N | 69E | 03 | SE OF SW | Nevada |
| Commodity | Importance |
|---|---|
| Tungsten Critical | Primary |
| Copper | Secondary |
| Lead | Secondary |
| Silver | Tertiary |
| Materials | Type of material |
|---|---|
| Calcite | Gangue |
| Epidote | Gangue |
| Garnet | Gangue |
| Quartz | Gangue |
| Result | FROM THE PLACER, .75% WO3. SAMPLE ASSAYED 8.0 OZ/T AG: 0.18% CU: 0.10% PB (1981). |
|---|
| Model code | 46 |
|---|---|
| USGS model code | 15a |
| Deposit model name | W veins |
| Host or associated | Associated | ||
|---|---|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Rock unit name | Corset Spring Shale;Johns Wash Limestone;Lincoln Peaks |
| Rock description | Corset Spring Shale;Johns Wash Limestone;Lincoln Peaks |
| (1) | -114.21251, 38.85134 |
|---|
| General form | TABULAR TO IRREGULAR |
|---|---|
| Thickness | 0.46M |
| Width | 0.36M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1916 |
| Year of first production | 1918 |
| District name | Lexington (Lexington Canyon, Shoshone) |
|---|
| Ownership category | National Forest |
|---|
| Type of workings | Surface/Underground |
|---|---|
| Length | 15.24M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M031259 |
HOSE, BLAKE & SMITH 1976, GEO & MIN RESOURCES OF WHITE PINE CO. NEV., NEV BUREAU OF MINES & GEO BULL 85
USBM, 1963, UNPUBLISHED DATA, NBMG FILE 332, ITEM 6.
STAGER, H.K., AND TINGLEY, J.V., 1988 TUNGSTEN DEPOSITS IN NEVADA; NBMG BULL. 105 P.219.
USBM, 1983, MILS DATA.
USBM, 1983, OPEN FILE REPORT MLA 68-83.
HOSE, ET AL 1976. STAGER, H.K., AND TINGLEY, J.V.,1988 TUNGSTEN DEPOSITS IN NEVADA; NBMG BULL. 105 P.219.
| Subject category | Comment text |
|---|---|
| Deposit | CALCITE VEINS UP TO 14 IN WIDE ALONG BEDDING. SCHEELITE OCCURS AS CRYSTALS IN THE CALCITE. A BLOCK 600 FT X 100 FTX 15 FT DEEP PROBABLY CONTAINS PLACER SCHEELITE. NUMEROUS QUARTZ AND CALCITE VEINS WITH SMALL BLEBS OF SULFIDE MINERALS AND MINOR AZURITE STAINING. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1979 | Giorgi, Albert John (Roberts, Ralph) | U.S. Geological Survey | |
| Updater | 01-OCT-1981 | La Pointe, D.D. (Tingley, J.V.) | U.S. Geological Survey | |
| Updater | 01-APR-1991 | Moyer, Lorre A. (Marcus, S.M.) | 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.