| Deposit ID | 10046535 |
|---|---|
| MRDS ID | M241712 |
| Record type | Site |
| Current site name | Jennie Mine |
| Alternate or previous names | NBMG Sample Site 1718 |
| Related records | 10125696 |
| Geographic coordinates: | -114.05026, 37.89858 (WGS84) |
|---|---|
| Elevation | 2103 |
Political divisions (FIPS codes)
Lincoln(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Deer Lodge Canyon(quadrangle 1:24,000 scale)
Caliente(quadrangle 1:100,000 scale)
Caliente(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Escalante Desert(hydrologic unit)
Escalante Desert-Sevier Lake(hydrologic accounting unit)
Escalante Desert-Sevier Lake(hydrologic subregion)
Great Basin(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Nevada | Lincoln |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 001N | 071E | 32 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Primary |
| Silver | Primary |
| Lead | Secondary |
| Copper | Secondary |
| Materials | Type of material |
|---|---|
| Cerargyrite | Ore |
| Gold | Ore |
| Calcite | Gangue |
| Pyrite | Gangue |
| Quartz | Gangue |
| Result | STOPE SAMPLE (1976) ASSAYED TR. AU, 0.2 OZ/T AG. SAMPLE 1718 CONTAINS 300 PPM MN, 2 PPM AG, 200 PPM BA, 30 PPM PB, 50 PPM ZR. |
|---|
| Model code | 150 |
|---|---|
| USGS model code | 25c |
| Deposit model name | Epithermal vein, Comstock |
| Mark3 model number | 16 |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite | ||||
| |||||
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite |
| (1) | -114.05026, 37.89858 |
|---|
| Type of structure | Local |
|---|---|
| Structure description | Fault, N80e, 55s, Displaces The Jennie Vein N Of The Shaft. Premineral Faulting, Also. |
| Strike | N10W-N15W |
|---|---|
| Dip | 55-70 NE |
| Thickness | 6.1M |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1901 |
| Year of first production | 1907 |
| Year of last production | 1948 |
| District name | Stateline/Gold Springs District |
|---|
| Ownership category | Private |
|---|
| Year | 1948 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1907-1948 | ||||||||||||||
| Material | AU | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^ 1.3 Oz/T Ag, Average Grade. | ||||||||||||||
| |||||||||||||||
| Year | 1948 | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1907-1948 | ||||||||||||||
| Material | ORE | ||||||||||||||
| Accuracy | Accurate | ||||||||||||||
| Description | Cp_Grade: ^0.22 Oz/T Au | ||||||||||||||
| |||||||||||||||
| Type of workings | Underground |
|---|---|
| Length | 243.84M |
| Overall depth | 91.44M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M241712 |
BENTZ, J. AND SMITH, P., 1983, FIELD EXAMINATION REPORT OF SEPT. 17, 1983.
PERRY, L.I., 1976, UTAH GEOLOGY VOL. 3, NO. 1, P. 23-49
THOMSON, K.C. AND PERRY, L.I., 1975, UTAH GEOLOGY, VOL. 2, NO. 1,
USGS P.P. 111, 1920, P. 565-567.
PERRY, L.I., 1976, P. 32
| Subject category | Comment text |
|---|---|
| Deposit | Discovery Year: 1900 OR EARLIER |
| Deposit | VEIN IS WELL EXPOSED IN NORTH WALL OF LOWER SHAFT WHERE IT FORMS A RESISTANT WHITE KNOB 7-10 FT WIDE. VEIN HAS SHARP BUT UNDULATORY CONTACTS WITH THE ALTERED ANDESITE WALLROCK, AND SHOWS SLIGHT "PINCH AND SWELL" SHAPE. IRON-STAINED ANDESITE ADJACENT TO THE VEIN IS FRACTURED AND VEINED PARALLEL TO THE MAIN VEIN ORIENTATION. VEINING OF THE WALL ROCK IS COMMON IN BOTH HANGING AND FOOT WALL EXPOSURES EXTENDING OUTWARD FROM MAIN VEIN ABOUT 5 FT. QUARTZ, CALCITE VEIN, AND QUARTZ VEIN WITH ANDESITE BRECCIA FRAGMENTS ARE THE MOST ABUNDANT ROCK TYPES ON THE LARGE DUMP. ALL VARIETIES OF QUARTZ-CALCITE COMBINATIONS EXIST, IE. QUARTZ REPLACING CALCITE, INTERGROWN WITH CALCITE, QUARTZ CUT BY OR CUTTING CALCITE VEIN. CALCITE IS GENERALLY WHITE, COARSELY CRYSTALLINE AND CONTAINS LITTLE FE. THE QUARTZ IS GENERALLY SUGARY OR MASSIVE, WHITE, AND ALSO OCCURS AS RADIATING OR PRISMATIC INTERLOCKING CRYSTALS IN VEINS AND BRECCIA. MOST VEINS ARE OPEN-CENTERED AND DRUSY QUARTZ FILLS VUGS AND FRACTURES OR |
| Deposit | REPLACES CALCITE. THE ALTERED ANDESITE FRAGMENTS CONTAINED IN THE VEIN ARE HIGHLY SILICIFIED AND STAINED WITH LIMONITE AFTER PYRITE. SOME OF THE FRAGMENTS SHOW A STOCK WORK OF VITREOUS QUARTZ VEINLETS |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-1984 | La Pointe, D.D. (Tingley, J.V.) | Nevada Bureau of Mines and Geology |
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.