| Deposit ID | 10014911 |
|---|---|
| MRDS ID | D012016 |
| Record type | Site |
| Current site name | Keystone Tunnels |
| Geographic coordinates: | -111.54106, 40.61855 (WGS84) |
|---|---|
| Elevation | 2789 |
| Relative position | 1800 FT N8W FROM JUPITER HILL |
Political divisions (FIPS codes)
Summit(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)
Lower Weber(hydrologic unit)
Weber(hydrologic accounting unit)
Great Salt Lake(hydrologic subregion)
Great Basin(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Utah | Summit |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Salt Lake | 002S | 004E | 30 | NE OF SE OF NW | Utah |
| Commodity | Importance |
|---|---|
| Lead | Primary |
| Silver | Primary |
| Zinc Critical | Primary |
| Gold | Secondary |
| Copper | Tertiary |
| Materials | Type of material |
|---|---|
| Chalcopyrite | Ore |
| Galena | Ore |
| Malachite | Ore |
| Sphalerite | Ore |
| Quartz | Gangue |
| Pyrite | Unknown |
| Result | AVERAGE GRADE WAS 0.15 OZ/TON AU, 5.04 OZ/TON AG, 11.20% PB, 4.50% ZN, |
|---|
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Plutonic Rock > Mafic Intrusive Rock > Diorite | ||||||
| Rock unit name | Crescent Dike | ||||||
| Rock description | Crescent Dike | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Rock unit name | Thaynes Formation;Ankarch Formation |
| Rock description | Thaynes Formation;Ankarch Formation |
| (1) | Alluvium and colluvium |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Uinta-Cottonwood Arch, Sevier Overthrust Belt, Iron Hollow Syncline |
| Type of structure | Local |
| Structure description | Crescent Fault Zone |
| General form | TABULAR |
|---|---|
| Strike | N 40 E TO N 60 E |
| Dip | 70 SE TO 40 SE |
| Depth to top | 0M |
| General form | TABULAR |
|---|---|
| Dip | 70 SE TO 40 SE |
| Development status | Past Producer |
|---|---|
| Commodity type | Metallic |
| Deposit size | Small |
| Significant | No |
| Discovery year | 1875 |
| Year of first production | 1923 |
| Year of last production | 1926 |
| District name | Park City District |
|---|
| Ownership category | Private |
|---|
| Type | Owner |
|---|---|
| Owner | Keystone Mining Co. |
| Year | 1926 | |||||||||||||||||||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Period | 1923-1926 | |||||||||||||||||||||||||||||||||||
| Accuracy | Estimate | |||||||||||||||||||||||||||||||||||
| Description | Cp_Grade: ^.15 Oz/Ton Au, 5.04 Oz/Ton Ag, 11.2% Pb, 4.5% Zn, | |||||||||||||||||||||||||||||||||||
| ||||||||||||||||||||||||||||||||||||
| Type of workings | Underground |
|---|---|
| Length | 525.78M |
| Overall depth | 73.15M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D012016 |
ERIKSON, A.J., (EDITOR), 1968, PARK CITY DISTRICT, UTAH: GUIDEBOOK TO THE GEOLOGY OF UTAH, NO. 22, UTAH GEOLOGICAL SOCIETY.
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, 672 PP.
BARNES, M.P., AND SIMOS, J.S., 1968, ORE DEPOSITS OF THE PARK CITY DISTRICT WITH A CONTRIBUTION ON THE MAYFLOWER LODE, IN ORE DEPOSITS OF THE UNITED STATES: AM. INST. METALL. ENG., V. II, P. 1102
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
| Subject category | Comment text |
|---|---|
| Deposit | PROPERTY STRADDLES THE CRESCENT FAULT ZONE WHICH IS COMPRISED OF NORTHEAST STRIKING FISSURES AND RELATED SPLAYS, AND NORTHEAST STRIKING PORPHYRY DIKES. MINERALIZATION OCCURS BOTH AS SMALL FISSURED/VEIN DEPOSITS WITHIN THE NORTHEAST STRIKING FAULT ZONE AND AS REPLACEMENT DEPOSITS WHICH HAVE REPLACED LIMESTONE HORIZONS IN THE THAYNES FORMATION. REPLACEMENT ARE PROBABLY MOST ABUNDANT IN THE FOOTWALL OF THE CRESCENT FAULT |
| Deposit | Discovery Year: 1870'S |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAY-1984 | Shubat, Michael A. | Utah Geological and Mineral Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.