| Deposit ID | 10095897 |
|---|---|
| MRDS ID | RE00032 |
| Record type | Site |
| Current site name | Calico Hills |
| Alternate or previous names | Calico, West Calico, Little Calico |
| Geographic coordinates: | -118.7618, 39.04741 (WGS84) |
|---|---|
| Relative position | SIX MILES NORTH OF SHURZ |
Political divisions (FIPS codes)
Mineral(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Weber Dam(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;014N | 029E | 03,04,05,06,07,08,09,10,11;31;32 | Nevada |
| Commodity | Importance |
|---|---|
| Iron | Primary |
| Copper | Primary |
| Lead | Primary |
| Zinc Critical | Primary |
| Molybdenum | Primary |
| Uranium | Primary |
| Chromium Critical | Primary |
| Boron-Borates | Secondary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Copper | Ore |
| Galena | Ore |
| Molybdenite | Ore |
| Pyrrhotite | Ore |
| Sphalerite | Ore |
| Actinolite | Gangue |
| Calcite | Gangue |
| Diopside | Gangue |
| Epidote | Gangue |
| Quartz | Gangue |
| Tremolite | Gangue |
| Wollastonite | Gangue |
| Zoisite | Gangue |
| Result | ASSAYS FROM DDL CA-1, FROM 1,374 FT. - 3,633 FT., AVERAGED 36.8% FE AND 0.093% CU, INCLUDING ONE 147 FT. SECTION THAT RAN 0.720% CU CERT REPORTS 420 PPM U (.05% U308) AND ANOMALOUS CR (CERT, P. 51) AG ASSAYS OF UP TO 1.602/T AND AU UP TO 0.035 OZ/T REPORTED BY SATKOSKI IN SEPARATE DDL. |
|---|
| Model code | 62 |
|---|---|
| USGS model code | 18d |
| Deposit model name | Skarn Fe |
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Rock unit name | Excelsior-Luning; |
| Rock description | Excelsior-Luning; |
| (1) | -118.7618, 39.04741 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Walker Lane |
| Type of structure | Local |
| Structure description | 2 Sets Of Faults: N20-40w, Related To Walker Lane; N10-30e, Possibly Resulting From Nw Faulting. |
| Strike | NW |
|---|---|
| Dip | 45SW |
| Thickness | 609.6M |
| Length | 1828.8M |
| Width | 457.2M |
| Depth to top | 134.11M |
| Depth to bottom | 609.6M |
| Development status | Occurrence |
|---|---|
| Commodity type | Both |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1956 |
| Discoverer | Columbia Iron Co./ Columbia Steel Company |
| Type | In-situ | |||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1967 | |||||||||||||||||||||
| Total resources | 272000000mt ore | |||||||||||||||||||||
| ||||||||||||||||||||||
| Type | In-situ | ||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Name | LAWRENCE & REDMOND | ||||||||||||||
| Estimate year | 1967 | ||||||||||||||
| Total resources | 600000000mt ore | ||||||||||||||
| |||||||||||||||
| Type | In-situ | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Estimate year | 1985 | ||||||||||||||||||||||||||||
| Total resources | 90702000mt ore | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | RE00032 |
JOHN, D.A., AND SHERLOCK, M.G., 1991, MAP SHOWING MINES AND PROSPECTS IN THE RENO 1 X 2 QUAD., NV AND CA, USGS MF 2154B, SYMBOL T7.
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, NV, USBM BIA REPT. 21-11.
COUNCIL OF ENERGY RESOURCES TRIBES, 1984, AN ASSESSMENT OF HYDROTHERMAL SYSTEMS ON PORTIONS OF THE WALKER RIVER RESERVATION, UNPUBL. REPORT 07-36-38-557.
TAYLOR, J., FOR TINGLEY, J., 1989, MINERAL COUNTY, CALICO HILLS, CALICO DEPOSIT, DRAFT MRDS RECORD (APPARENTLY NEVER ENTERED), NBMG UNPUBLISHED MINING DISTRICT (TINGLEY) FILES
LAWRENCE, E.F., 1969, GEOLOGICAL AND GEOPHYSICAL INVESTIGATIONS OF THE MINERAL DEPOSITS OF THE CALICO AREA, MINERAL COUNTY, NEVADA, UNIVERSITY OF CALIFORNIA, RIVERSIDE, PH.D. DISSERTATION
LAWRENCE, E.F., REDMOND, R.L., 1967, EXPLORATION OF THE CALICO AREA, WALKER RIVER INDIAN RESERVATION, MINERAL COUNTY, NV, SME PREPRINT 67-I-311
BOTH 1967 ESTIMATES ARE FOR "INFERRED RESERVES" FROM CERT, P. 50. 1985 FIGURE FROM DRAFT MRDS RECORD IN TINGLEY FILES (NO SOURCE GIVEN)
| Subject category | Comment text |
|---|---|
| Deposit | THE IP AND DRILLING "DISCLOSED EXTENSIVE MINERALIZATION AT DEPTHS OF 400 FT. ON THE NORTHWEST END AND OVER 1,000 FT. TO THE SOUTHEAST," (LAWRENCE). DRILL HOLE CA-1 CUT THE PRE-TERTIARY/VOLCANIC CONTACT AT 1,308 FT. SKARN AND HORNFELS WERE FOUND IN ALL MARTEL DRILL HOLES. SKARN WAS ALSO REPORTED ON SURFACE IN SEC. 31 (LAWRENCE). CALCITE-GTZ-PY-CHALCOPYRITE/VEINLETS CUT THE SKARN. POSSIBLY 2 MINERALIZING EVENTS, AN EARLIER FE-MN EVENT, AND LATER CU+PB+ZN, ETC. EVENT. |
| Deposit | THE DEPOSIT WAS INITIALLY IDENTIFIED BY GEOPHYSICAL SURVEYS. 10 MILES OF STRIKE-SLIP FAULTING MAY HAVE SEPARATED THE CALICO AND HOTTENTOT DEPOSITS. ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1992 | Marcus, S. | U.S. Geological Survey | |
| Updater | 01-AUG-1993 | Marcus, 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.