Kentucky Derby Mine

The Kentucky Derby Mine is a copper, gold, and silver mine located in Albany county, Wyoming at an elevation of 9,301 feet.

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: Kentucky Derby Mine  

State:  Wyoming

County:  Albany

Elevation: 9,301 Feet (2,835 Meters)

Commodity: Copper, Gold, Silver

Lat, Long: 41.28611, -106.17944

Map: View on Google Maps

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.


Satelite image of the Kentucky Derby Mine

Mine Description

The Kentucky Derby workings are situated in the shear zone along upper Middle Fork near the waterfall which marks an abrupt change in stream flow direction. A short crosscut penetrates strongly shattered and sulphide enriched, dark, dense shear zone tectonites. The mineralized zone has been appreciably oxidized and the sulphide masses are characteristically coated with films of limonite and alum. The platinum group metals osmium, palladium, iridium, and platinum along with gold have been reported from these ores. NRRI assays of grab samples collected from the adit show the presence of copper, gold, and silver, but no platinum group metals were recognized.

Source: The Centennial Ridge Gold-Platinum District, Albany County, Wyoming, 1968. The Geological Survey of Wyoming.

Kentucky Derby Mine MRDS details

Site Name

Primary: Kentucky Derby Mine
Secondary: Centennial Ridge District


Commodity

Primary: Copper
Primary: Gold
Primary: Silver
Secondary: Iridium
Secondary: Osmium
Secondary: Palladium
Secondary: Platinum


Location

State: Wyoming
County: Albany
District: Centennial Ridge District


Land Status

Land ownership: National Forest
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

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Underground
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

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


Mineral Deposit Model

Not available


Orebody

Form: VEINS


Structure

Type: R
Description: Mullen Creek-Nash Fork Shear Zone

Type: L
Description: Shear Zones


Alterations

Alteration Type: L
Alteration Text: Mineralized Zone Has Been Oxidized


Rocks

Name: Tectonite
Role: Host
Age Type: Host Rock
Age Young: Neoproterozoic

Name: Tectonite
Role: Host
Age Type: Associated Rock Unit
Age Young: Neoproterozoic


Analytical Data

Analytical Data: AU=TR, AG=0.69 PPM, IR=TR, PD=TR, OS=TR, PT=0.11 PPM. PT=3.5 PPM IN ROCK SAMPLE (ALL VALUES CONVERTED TO PPM FROM OZ/TON)


Materials

Ore: Chrysocolla
Ore: Malachite
Ore: Pyrite
Ore: Gold
Ore: Chalcopyrite
Gangue: Limonite


Comments

Comment (Deposit): ORE OCCURS IN SULFIDE-RICH ZONES; UNPUBLISHED MODEL NAME: NEW RAMBLER CU-AU-PGE.

Comment (Production): NO PRODUCTION FIGURES AVAILABLE; SMALL PRODUCTION PRESUMED

Comment (Workings): SHORT CROSSCUTS

Comment (Deposit): "The Kentucky Derby workings are situated in the shear zone along upper Middle Fork near the waterfall which marks an abrupt change in stream flow direction. A short crosscut penetrates strongly shattered and sulphide enriched, dark, dense shear zone tectonites. The minerized zone has been appreciably oxidized and the sulphide masses are characteristically coated with films of limonite and alum. The platinum group metals osmium, palladium, iridium, and platinum along with gold have been reported from these ores (see Table 1). NRRI assays of grab samples collected from the adit show the presence of copper, gold, and silver, but no platinum group metals were recognized." (McCallum, 1968, p. 10)


References

Reference (Deposit): HAUSEL, W.D., 1989, THE GEOLOGY OF WYOMING'S PRECIOUS METAL LODE AND PLACER DEPOSITS: GEOLOGICAL SURVEY OF WYOMING BULLETIN 68, P. 99.
Pages: p. 99.

Reference (Deposit): HAUSEL, 1980, GOLD DISTRICTS OF WYOMING: GEOLOGICAL SURVEY OF WYOMING REPORT OF INVESTIGATIONS 23, P. 36.
Pages: p. 36.

Reference (Deposit): MCCALLUM, M.E., 1968, THE CENTENNIAL RIDGE GOLD-PLATINUM DISTRICT, ALBANY COUNTY, WYOMING: GEOLOGICAL SURVEY OF WYOMING PRELIMINARY REPORT 7, P. 9, 10.
Pages: p. 10, pl. 1.


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