| Deposit ID | 10040609 |
|---|---|
| MRDS ID | M055445 |
| Record type | Site |
| Current site name | East China Pit |
| Alternate or previous names | Devil's Corral Pit, NBMG Sample Sites 2704,2705, 2706 |
| Related records | 10246680, 10040610 |
| Geographic coordinates: | -118.66432, 40.86044 (WGS84) |
|---|---|
| Elevation | 1433 |
| Relative position | 2 MILES SE OF SULPHUR |
Political divisions (FIPS codes)
Humboldt(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Sulphur(quadrangle 1:24,000 scale)
Eugene Mountains(quadrangle 1:100,000 scale)
Lovelock(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Lower Quinn(hydrologic unit)
Black Rock Desert(hydrologic accounting unit)
Black Rock Desert-Humboldt(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 | Humboldt |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 035N | 029E | 35 | Nevada |
| Commodity | Importance |
|---|---|
| Sulfur | Primary |
| Mercury | Secondary |
| Gold | Tertiary |
| Materials | Type of material |
|---|---|
| Cinnabar | Ore |
| Sulfur | Ore |
| Alunite | Gangue |
| Clay | Gangue |
| Quartz | Gangue |
| Result | SAMPLE 2704 OF MOST INTENSELY ALTERED CONGLOMERATE CONSISTING OF QUARTZ AND ANHYDRITE CONTAINS 0.05 % FE, 0.05 % M-G, 20 % CA, 0.1 % TI, 700 PPM BA, 5 PPM NI, 500 PPM SR, 50 PPM- ZR. SAMPLE 2705 OF MODERATELY ALTERED CONGLOMERATE CONSISTING- OF QUARTZ AND SULFUR CONTAINS 0.3 % TI, 500 PPM BA,5 PPM NI, -AND 200 PPM ZR. SAMPLE 2706 OF ALTERED ROCK ADJACENT TO SULFUR- BODY CONSISTING OF QUARTZ AND CRISTOBALITE, CONTAINS 0.05 % F-E, 0.02 % MG, 0.2 % TI, 20 PPM B, 1500 PPM BA, 10 PPM CR, 10 P-PM CU, 5 PPM NI, 700 PPM ZR. |
|---|
| Model code | 104 |
|---|---|
| USGS model code | 25a |
| Deposit model name | Hot-spring Au-Ag |
| Mark3 model number | 45 |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone | ||
| |||
| (1) | Older gravels |
|---|
| Length | 1981.2M |
|---|---|
| Width | 548.64M |
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| District name | Sulphur District |
|---|
| Ownership category | Private |
|---|
| Type | Owner-Operator |
|---|---|
| Owner | Pacific Sulphur Inc. |
| First year | 1967 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M055445 |
GALLAGHER, M. J., 1967, NEVADA MINES, MILLS AND SMELTERS IN OPERATION AS OF JULY 1, 1967: STATE INSPECTOR OF MINES, CARSON CITY, NEVADA, PAMPHLET, 16 P.
PAPKE, K. G., 11 SEP 84, NBMG FIELD EXAMINATION AND SAMPLE ANALYSES.
QUADE, JACK, 2 SEP 84, NBMG FIELD EXAMINATION AND SAMPLE ANALYSIS
NBMG STAFF, 1985, NBMG OFR 85-3.
| Subject category | Comment text |
|---|---|
| Deposit | DRILLING OPERATIONS ACTIVE JUST NE OF HERE ABOUT 0.5 MILE FOR GOLD. SAMPLE 1795 WAS FROM SAME AREA AS OTHER SAMPLE-S AND CONTAINS DARK REDDISH BROWN HIGHLY ALTERED RHYOLITE BREC-CIA WITH SULPHUR AND POSSIBLE SULFIDES. ANALYSIS SHOWS 0.5 % F-E, 0.03 % MG, 0.15 % CA, 0.7 % TI, 10 PPM MN, 50 PPM B, 1500 P-PM BA, 20 PPM NB, 30 PPM PB, 7 PPM SC, 50 PPM V, 15 PPM Y, +10-00 PPM ZR. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT; 3 FIELD OBSERV |
| Deposit | SULFUR OCCURS AS DISSEMINATED GRAIN, PREFERENTIAL REPLACEMENT OF CONGLOMERATE MATRIX, IRREGULAR VEINS AND MASSES, -AND COATINGS ON FRACTURE SURFACES. MERCURY IS PRESENT IN SOME -OF THE MATERIAL, AS IS SILVER. IN THE BIG PIT, ALL ROCKS ARE M-ODERATELY TO STRONGLY ALTERED, BUT CONGLOMERATE CLASTS ARE COM-MONLY RECOGNIZABLE. MUCH OF THE ROCK CONTAINS LITTLE OR NO SUL-FUR. SULFUR IS CONCENTRATED IN 3 OR 4 IRREGULAR AREAS UP TO 20- FT ACROSS WHERE IT MAKES UP PERHAPS ONE-FIFTH OF THE ROCK. WI-THIN THESE AREAS SOME SMALL BODIES ARE QUITE PURE. MOST STRING-ERS OF SULFUR ARE SEMI-HORIZONTAL, PROBABLY REFLECTING BEDDING- ATTITUDE WHICH OTHERWISE IS NOT VISIBLE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1976 | Gassaway, Judith S. | Nevada Bureau of Mines and Geology | |
| Updater | 01-APR-1986 | La Pointe, D.D. (Tingley, J.V.) | Nevada Bureau of Mines and Geology | |
| Updater | 01-APR-1981 | Lapointe D. D. | 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.
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