Copper King Mine Adams

The Copper King Mine Adams is a gold and copper mine located in Laramie county, Wyoming.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Copper King Mine Adams  

State:  Wyoming

County:  Laramie

Elevation:

Commodity: Gold, Copper

Lat, Long: 41.14472, -105.18556

Map: View on Google Maps

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Satelite image of the Copper King Mine Adams

Copper King Mine Adams MRDS details

Site Name

Primary: Copper King Mine Adams
Secondary: Arizona Mine
Secondary: Bartlett Copper King
Secondary: CK Gold
Secondary: Copper King Mine
Secondary: Silver Crown District


Commodity

Primary: Gold
Primary: Copper
Tertiary: Silver


Location

State: Wyoming
County: Laramie
District: Silver Crown District


Land Status

Land ownership: Private
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.


Holdings

Not available


Workings

Type: Underground


Ownership

Owner Name: Compass Resources Ltd
Percent: 5.00
Years: 2002 -

Owner Name: Mountain Lake Resources Inc
Percent: 100.0
Info Year: 2010
Years: 2002 -

Owner Name: Copper King Mining Company
Home Office: Cheyenne, WY
Info Year: 1952


Production

Not available


Deposit

Record Type: Deposit
Operation Category: Past Producer
Deposit Type: Porphyry Cu-Au
Operation Type: Surface
Year First Production: 1881
Discovery Year: 1879
Years of Production:
Organization:
Significant: Y
Deposit Size: S


Physiography

General Physiographic Area: Rocky Mountain System
Physiographic Province: Southern Rocky Mountains


Mineral Deposit Model

Model Name: Porphyry Cu-Au


Orebody

Form: HYDROTHERMAL DISSEMINATED; STOCKWORK BROAD DISSEMINATED ZONE IN NEAR VERTICAL SHEAR ZONE


Structure

Type: L
Description: Faults

Type: L
Structure: BROAD E-W TRENDING MYLONITE ZONE


Alterations

Alteration Type: L
Alteration: POTASSIC, PHYLLIC


Rocks

Not available


Analytical Data

Analytical Data: Assayed about 3% Cu
Analytical Data: AT THE 80 FT AND 130 FT LEVELS CONTAINED 11% CU AND 2.5 OZ AU. LES S THAN 1% CU AT SURFACE
Analytical Data: FOURTEEN SAMPLES TAKEN BY JAMISON (1912) 0.22 TP 2.43% CU, 0.06 TO 0.42 OPT AU, AND 0.4 TO 0.8 OPT AG


Materials

Ore: Copper
Ore: Sphalerite
Ore: Azurite
Ore: Chrysocolla
Ore: Malachite
Ore: Molybdenite
Ore: Cuprite
Ore: Bornite
Ore: Pyrite
Ore: Chalcopyrite
Gangue: Epidote
Gangue: Fluorite
Gangue: Magnetite
Gangue: Limonite
Gangue: Hematite
Gangue: Barite


Comments

Comment (Deposit): HOST ROCK FOLIATED GRANODIORITE IS PROBABLY BOULDER CREEK EQUIVALENT. ALTERATION AND MINERALIZATION WAS RELATED TO LATEST STAGES OF SHERMAN GRANITE BUT PREDATED THE EMPLACEMENT OF SPARSE PEGMATITES. MINERALIZED SHEAR ZONES IN THE COPPER KING DEPOSITS APPEAR TO HAVE DEVELOPED UNDER DUCTILE CONDITIONS. THE EAST WEST SHEAR ZONE AT THE DEPOSIT CHANNELED HIGH TEMPERATURE POTASH AND METAL RICH HYDROTHERMAL INTO THE COUNTRY ROCK. LATE STAGE SHERMAN FELSIC DIKES WERE ALSO MINERALIZED PLACING THE HYDROTHERMAL EVENT AT THE LATEST STAGES OF SHERMAN RELATED THERMAL ACTIVITY. MAGNETITE IS ABUNDANT IN THE MINERALIZED ZONE INDICATING HIGH TEMPERATURE RELATIVELY OXIDIZING CONDITIONS, MAGNETITE IS USUALLY ALTERED AT GRAIN BOUNDARIES TO MARTITIE (HEMATITE) INDICATING AN INCREASE IN OXIDATION POST DATED THE ORE FORMING EVENT..

Comment (Deposit): BROAD DISSEMINATED COPPER SULFIDES ZONE FOLLOWS DUCTILE SHEAR ZONE. LOCALLY MINERALIZATION IS STOCKWORK. ALTERATION CONSISTS OF LOCAL INTENSE SILICA FLOODING, KSPAR AND BIOITITE POTASSIC ALTERATION SURROUNDED BY PROPYLITIC ALTERATION CONSISTING OF CHLORITE AND EPIDOTE. THE DEPOSITS HAS BEEN CHARACTERIZED AS A PROTEROZOIC PORPHYRY DEPOSIT. HOWEVER THE MAIN HOST IS NOT EXCLUSIVELY THE SHERMAN GRANITE. THE SHERMAN GRANITE PROVIDED THE HEAT AND FLUIDS BUT THE MINERALIZATION IS IN PART A REPLACEMENT OF THE COUNTRY ROCK, AN OLDER (1.7 B.Y.) DEFORMED GRANODIORITE. E-W TRENDING SHEAR ZONE THAT IS PERPENDICULAR TO THE CONTACT WITH THE COUNTRY ROCK GRANODIORITE AND THE SHERMAN BATHOLITH. THIS SHEAR FOCUSED HYDROTHERMAL FLUIDS AND CONTROLLED INTRUSION OF LATE STAGE FELSIC DIKES

Comment (Exploration): SEVERAL OTHER LARGE GEOPHYSICAL AND GEOCHEMICAL ANOMALIES OCCUR SOUTHEAST AND SOUTHWEST OF THE MAIN ZONE. EXTENSIVE DRILLING HAS BEE COMPLETED WITH AT LEAST 10,000 FT OF DIAMOND DRILLING COMPLETED.

Comment (Workings): 157 FOOT SHAFT WITH 102 FT OF DRIFTS AT THE 80 FT LEVEL AND 260 FT OF DRIFTS ON THE 130 FT LEVEL AS WELL AS SEVERAL LARGE STOPES.


References

Reference (Deposit): Klein, Terry, 1974, Geology and mineral deposits of the Silver Crown Mining District, Laramie County, Wyoming: Geological Survey of Wyoming Preliminary Report No. 14, 27 p., 2 pls.
Pages: p. 15, 21.

Reference (Deposit): DMEA Docket No. 2655, 110 p., http://minerals.usgs.gov/dockets/scans/wy/dmea/2655_DMEA.pdf
URL: http://minerals.usgs.gov/dockets/scans/wy/dmea/2655_DMEA.pdf

Reference (Deposit): USGS RI 5139

Reference (Reserve-Resource): Pay Dirt, 1999

Reference (Geology): Hausel, W.D., 1997, Copper,Lead,Zinc,Molybdenum,and Associated Metal Deposits of Wyoming: Wyoming State Geological Survey, Bulltin 70. 227 p

Reference (Development): Caledonia Resources Ltd Annual Report 1984 Caledonia Reources Ltd Report To Shareholders 2/85 Caledonia Resources Ltd Report To Shareholders 7/29/86 Caledonia Resources Ltd News Release 5/12/87 Aston Resources Ltd Annual Report 1987 (7/14/88) Royal Gold Inc Press Release 2/28/89 Compass Resources NL Quarterly Report 12/31/94 Compass Resources NL Quarterly Report 12/31/95 Mountain Lake Resources Inc 6/97 Annual Report 10/14/97 Mountain Lake Resources Inc 6/97 Annual Report 10/31/02

Reference (Deposit): GSW BULL 50, P. 88


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