Last Chance

The Last Chance is a lead, copper, zinc, and silver mine located in Okanogan county, Washington at an elevation of 2,999 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: Last Chance

State:  Washington

County:  Okanogan

Elevation: 2,999 Feet (914 Meters)

Commodity: Lead, Copper, Zinc, Silver

Lat, Long: 48.49167, -119.74000

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 Last Chance

Last Chance MRDS details

Site Name

Primary: Last Chance
Secondary: Ruby Lode Claim


Commodity

Primary: Lead
Primary: Copper
Primary: Zinc
Primary: Silver


Location

State: Washington
County: Okanogan
District: Conconully, Ruby Hill Area


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Years of Production:
Organization:
Significant: N


Physiography

General Physiographic Area: Pacific Mountain System
Physiographic Province: Cascade-Sierra Mountains
Physiographic Section: Northern Cascade Mountains


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Type: R
Description: The Quartz Monzonite Was Probably Emplaced In A Magmatic Arc.


Alterations

Not available


Rocks

Not available


Analytical Data

Not available


Materials

Ore: Sphalerite
Ore: Tetrahedrite
Ore: Galena
Ore: Chalcopyrite
Gangue: Pyrite
Gangue: Quartz


Comments

Comment (Location): AT THE NORTH END OF RUBY HILL

Comment (Geology): THE VEIN IS IN GRANODIORITE OF CRETACEOUS AGE NEAR THE CONTACT WITH HORNBLENDE-BIOTITE SCHIST OF THE METAMORPHIC COMPLEX OF CONCONULLY (GULICK AND KOROSEC, 1990, GEOL. MAP).

Comment (Production): ORE WAS BLOCKED OUT BUT WAS NOT MINED BECAUSE OF THE SILVER PANIC OF 1883. IN 1920 THE MINE WAS REOPENED, AND ORE THAT AVERAGED 30 OZ/TON AG, 17% PB, AND 4% CU WAS SHIPPED TO A SMELTER AT BRADLEY, IDAHO. SMALL SHIPMENTS OF ORE WERE MADE AGAIN IN 1921 AND 1924 (MOEN, 1973, P. 18).


References

Reference (Deposit): DERKEY, R.E.; JOSEPH, N.L.; LASMANIS, R., 1990, METAL MINES OF WASHINGTON-PRELIMINARY REPORT: STATE OF WASHINGTON, DEPARTMENT OF NATURAL RESOURCES, DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN-FILE REPORT 90-18, 577 P.

Reference (Deposit): GULICK, C.W.; KOROSEC, M.A., COMPILERS, 1990, GEOLOGIC MAP OF THE OMAK 1:100,000 QUADRANGLE, WASHINGTON: WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN-FILE REPORT 90-12, 52 P., 1 PL.

Reference (Deposit): HUNTTING, M. T., 1956, INVENTORY OF WASHINGTON MINERALS-PART II, METALLIC MINERALS: WASHINGTON DIVISION OF MINES AND GEOLOGY BULLETIN 37, V. 1, 428 P.; V. 2, 67 P.

Reference (Deposit): MOEN, W.S., 1973, CONCONULLY MINING DISTRICT OF OKANOGAN COUNTY, WASHINGTON: WASHINGTON DIVISION OF MINES AND GEOLOGY INFORMATION CIRCULAR 49, 42 P.

Reference (Deposit): PATTY, E.N., 1921, THE METAL MINES OF WASHINGTON: WASHINGTON GEOLOGICAL SURVEY BULLETIN 23, 366 P.


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