| Deposit ID | 10037403 |
|---|---|
| MRDS ID | M035031 |
| Record type | Site |
| Current site name | Reservation Hill |
| Alternate or previous names | So Central Section 18 Prospect, Se Sec 18 Prospect, Nmbg Sample Sites 3777, 3778 |
| Geographic coordinates: | -118.90014, 39.00574 (WGS84) |
|---|---|
| Elevation | 1463 |
| Relative position | 6 MILES NW OF SHURZ |
Political divisions (FIPS codes)
Mineral(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Weber Reservoir(quadrangle 1:24,000 scale)
Fallon(quadrangle 1:100,000 scale)
Reno(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Walker(hydrologic unit)
Walker(hydrologic accounting unit)
Central Lahontan(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
BIA(Federal land areas administered by BIA)
| Country | State | County |
|---|---|---|
| United States | Nevada | Mineral |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 013N | 027;028E | 1,12;6,7 | Nevada |
| Commodity | Importance |
|---|---|
| Gold | Secondary |
| Lead | Secondary |
| Zinc Critical | Secondary |
| Silver | Secondary |
| Materials | Type of material |
|---|---|
| Pyrite | Ore |
| Magnetite | Gangue |
| Quartz | Gangue |
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| (1) | -118.90014, 39.00574 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Walker Lane |
| Strike | E |
|---|---|
| Dip | 40N |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Type of workings | Surface/Underground |
|---|---|
| Overall depth | 9.14M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M035031 |
QUADE, J., 1989, RESERVATION HILL, UNPUBLISHED DRAFT CRIB RECORD, MINERAL COUNTY, MOUNTAIN VIEW DISTRICT, SITE REPORT 6-12-89: NBMG UNPUBLISHED MINING DISTRICT (J. TINGLEY) FILES
JOHN, D.A., AND SHERLOCK, M.G., 1991, MAP SHOWING MINES AND PROSPECTS IN THE RENO 1 BY 2 QUADRANGLE, NEVADA AND CALIFORNIA: USGS MF-2154-B, SYMBOL # T5
SATKOSKI, J.J. , LAMBETH, R.H., WHITE, W.W., AND DUNN, M.D., 1985, FIELD INVENTORY OF THE MINERAL RESOURCES AND COMPILATION OF EXPLORATION DATA, WALKER RIVER INDIAN RESERVATION, NEVADA: USBM, BIA REPORT 21-11
SCHRADER, F.C., 1947, CARSON SINK AREA, NEVADA, USGS UNPUBLISHED REPORT BASED ON FIELDWORK 1911-1920, P292-295, IN NBMG FILES
RESERVATION HILL, UNPUBLISHED DRAFT CRIB RECORD, MINERAL COUNTY, MOUNTAIN VIEW DISTRICT: NBMG UNPUBLISHED MINING DISTRICT (J. TINGLEY) FILES
| Subject category | Comment text |
|---|---|
| Deposit | J. QUADE TOOK NBMG SAMPLES 3777, 3778. MRDS DRAFT RECORD BY J. TAYLOR FOR J. TINGLEY (NBMG), DATED 89 09, APPARENTLY NEVER ENTERED. SATOSKI AND OTHERS STATE THAT RESERVATION HILL "MAY BE" IN THE SAME AREA AS SCHRADER'S BENWAY DISTRICT, YET SATKOSKI DID NOT FIND MINERALS LIKE CERARGYRITE MENTIONED BY SCHRADER. THE BENWAY DISTRICT IS NE OF RESERVATION HILL ( SEE MRDS RECORD FOR AFTERTHOUGHT). THEREFORE, ANY DISCUSSION OF SCHRADER'S BENWAY DATA ARE NOT MENTIONED IN THIS RESERVATION HILL RECORD. THIS RECORD IS CONSTRUCTED FROM DIRECT SITE OBSERVATIONS AT RESERVATION HILL BY SATKOSKI AND OTHERS, AND QUADE. NO EVIDENCE OF PROSPECTS IN SECTION 2, T13N, R27W (SATKOSKI, P156), SO SECTION 1 PROBABLY CORRECT. |
| Deposit | THIS RECORD INCLUDES INFORMATION FROM MRDS RECORD #M035029, WHICH HAS BEEN DELETED |
| Deposit | 3 TYPES OF MINERALIZATION, FROM OLDEST TO YOUNGEST ARE DESCRIBED BY SATKOSKI: (1) CONTACT METASOMATIC WITH E-W, EN ECHELON QUARTZ-VEIN-FILLED SHEAR ZONES THAT DIP 40N; (2) N-S TO NW VEINS AND BRECCIAS ASSOCIATED WITH APLITE OR LATITE DIKES; (3) METALLIFEROUS, UNCONFORMABLE CONTACT BETWEEN TERTIARY TUFF AND TRIASSIC METASEDIMENTARY ROCKS. SATKOSKI POSTULATES THAT MAGNETITE IN TYPE 1 IS CRETACEOUS OR OLDER. TYPE 2 VEINS FILL WALKER LANE TYPE STUCTURES AND HAVE BEEN SUBJECTED TO SEVERAL PERIODS OF MOVEMENT. SHEAR ZONES FILLED BY TYPE 2 VEINS HAVE BEEN BRECCIATED, INTRUDED BY LATITE (?) DIKES, THEN BRECCIATED AGAIN. VEINS ARE UP TO SEVERAL INCHES THICK IN INDIVIDUAL SHEAR ZONES THAT ARE A FEW FEET TO TENS OF FEET WIDE. THE SHEAR ZONES ARE COLLECTIVELY UP TO SEVERAL HUNDRED FEET THICK. TYPE 2 VEINS "ARE PROBABLY YOUNGER THAN 30 MYBP." "METALLIZED FLUIDS" MAY HAVE MIGRATED ALONG THE TYPE 3 CONTACT AFTER THE TUFF DEPOSITION (AFTER 30 MYBP). TYPE 3 MAY BE RELATED TO WALKER LANE FAULTS, |
| Deposit | "BUT MORE LIKELY IS RELATED TO GEOTHERMAL CELLS ASSOCIATED WITH BASIN RANGE FAULTING." QUOTES AND INFORMATION ALL FROM SATKOSKI AND OTHERS, 1985. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1978 | Fiebelkorn, J. B. (Stewart, J. H.) | U.S. Geological Survey | |
| Updater | 01-AUG-1993 | Marcus, Susan | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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