| Deposit ID | 10106660 |
|---|---|
| MRDS ID | D011924 |
| Record type | Site |
| Current site name | Iowa Copper Mine |
| Alternate or previous names | Silver King Western |
| Geographic coordinates: | -111.56884, 40.61744 (WGS84) |
|---|---|
| Elevation | 2746 |
| Relative position | 2500 FT S8W FROM SCOTT HILL |
Political divisions (FIPS codes)
Salt Lake(county)
Utah(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Brighton(quadrangle 1:24,000 scale)
Salt Lake City(quadrangle 1:100,000 scale)
Salt Lake City(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Jordan(hydrologic unit)
Jordan(hydrologic accounting unit)
Great Salt Lake(hydrologic subregion)
Great Basin(hydrologic region)
Federal lands
Uinta-Wasatch-Cache National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Utah | Salt Lake |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Salt Lake | 002S | 003E | 25 | NW OF SW OF NW | Utah |
| Commodity | Importance |
|---|---|
| Copper | Primary |
| Gold | Primary |
| Silver | Primary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Chrysocolla | Ore |
| Malachite | Ore |
| Hematite | Gangue |
| Limonite | Gangue |
| Pyrite | Gangue |
| Quartz | Gangue |
| Result | OVERALL GRADE OF ORE IS 6.3% CU, .051 OZ/TON AU, 3.53 OZ/TON AG |
|---|
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale | ||
| Rock unit name | Park City Formation;Woodside Shale | ||
| Rock description | Park City Formation;Woodside Shale | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| (1) | -111.56884, 40.61744 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Uinta-Cottonwood Arch, Cordilleran Hingeline, Sevier Overthrust Belt |
| Type of structure | Local |
| Structure description | Several Northeast Striking Normal Faults |
| General form | POD |
|---|---|
| Strike | N25E TO N75E |
| Dip | 45 SE TO 70 NW |
| Thickness | 1.52M |
| Depth to top | 0M |
| General form | POD |
|---|---|
| Dip | 45 SE TO 70 NW |
| Development status | Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1875 |
| Year of first production | 1906 |
| Year of last production | 1920 |
| District name | Big Cottonwood District |
|---|
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | Silver King Western Manufacturing Co. |
| Home office | Salt Lake City, UT |
| Year | 1920 | ||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1909-1920 | ||||||||||||||||||||||||||||
| Material | ORE | ||||||||||||||||||||||||||||
| Accuracy | Estimate | ||||||||||||||||||||||||||||
| Description | Cp_Grade: ^6.3% Cu, .051 Oz/Ton Au, 3.53 Oz/Ton Ag | ||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||
| Type of workings | Surface/Underground |
|---|---|
| Length | 914.4M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D011924 |
JAMES, L.P., 1979, GEOLOGY, ORE DEPOSITS, AND HISTORY OF THE BIG COTTONWOOD MINING DISTRICT, SALT LAKE COUNTY, UTAH: U.G.M.S. BULL. NO. 114.
BUTLER, B.S., LOUGHLIN, G.F., HEIKES, V.C., AND OTHERS, 1920, THE ORE DEPOSITS OF UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER, NO. 111.
BAKER, A.A., CALKINS, F.C., CRITTENDEN, M.D., JR., AND BROMFIELD, C.S., 1966, GEOLOGIC MAP OF THE BRIGHTON QUADRANGLE, UTAH: U.S. GEOLOGICAL SURVEY GEOL. QUAD. MAP GQ-534
JAMES, L.P., 1979
| Subject category | Comment text |
|---|---|
| Deposit | SEVERAL NORTHEAST STRIKING FRACTURES APPEAR TO HAVE SUPPLIED SOLUTIONS WHICH CAUSED REPLACEMENT-TYPE MINERALIZATION IN CALCAREOUS BEDS NEXT TO FRACTURES. DOMINANT TYPE OF MINERALIZATION IS REPLACEMENT-TYPE. THIS AREA IS SOMEWHAT UNIQUE IN THAT THE DOMINANT ORES ARE CU AND AU AND ALTERATION AT THE SURFACE CONSISTS OF SILICIFIED, IRON-STAINED BRECCIAS. |
| Deposit | Discovery Year: 1870'S |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1984 | Shubat, Michael A. | Utah Geological and Mineral Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.