Spokane

The Spokane is a gold, silver, lead, zinc, and copper mine located in Okanogan county, Washington.

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: Spokane  

State:  Washington

County:  Okanogan

Elevation:

Commodity: Gold, Silver, Lead, Zinc, Copper

Lat, Long: 48.37389, -120.15444

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 Spokane

Spokane MRDS details

Site Name

Primary: Spokane
Secondary: Gold Crown


Commodity

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


Location

State: Washington
County: Okanogan


Land Status

Not available


Holdings

Not available


Workings

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Deposit Type: Vein
Operation Type: Unknown
Year Last Production: 1941
Years of Production:
Organization:
Significant: N
Deposit Size: S


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 Newby Group Was Deposited At Or Near Volcanic Island Arcs.


Alterations

Not available


Rocks

Name: Dacite
Role: Host
Age Type: Host Rock Unit
Age Young: Late Cretaceous

Name: Dacite
Role: Host
Age Type: Associated Rock Unit
Age Young: Late Cretaceous


Analytical Data

Not available


Materials

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


Comments

Comment (Location): ON TWISP RIVER ROAD, 2 MILES WEST OF TWISP.

Comment (Production): SMALL AMOUNTS OF ORE WERE SHIPPED IN 1939 AND 1954. SIX TONS SHIPPED IN 1941 CONTAINED 0.40 OZ/TON AU, 20.25 OZ/TON AG, 4.5% ZN, AND 3.8% PB (HUNTTING, 1956, P. 149; BURNET, 1976, TABLE 2).

Comment (Geology): MINERALIZATION IS IN SILICIFIED DACITE BRECCIA OF THE JURASSIC-CRETACEOUS NEWBY GROUP; IN PLACES THE NEWBY GROUP IS CONTACT METAMORPHOSED BY THE ALDER CREEK STOCK, WHICH WAS DATED AT 137 -+ 4 M.Y. (BURNET, 1976; BUNNING, 1990).


References

Reference (Deposit): BANTA, H.E., 1956, DIRECTORY OF WASHINGTON MINING OPERATIONS, 1956: WASHINGTON DIVISION OF MINES AND GEOLOGY INFORMATION CIRCULAR 25, 87 P.

Reference (Deposit): BUNNING, B.B., COMPILER, 1990, GEOLOGIC MAP OF THE EAST HALF OF THE TWISP 1:100,000 QUADRANGLE, WASHINGTON: WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN-FILE REPORT 90-9, 51 P., 1 PL.

Reference (Deposit): BURNET, F.W., 1976, FELSIC VOLCANIC ROCKS AND MINERAL DEPOSITS IN THE BUCK MOUNTAIN FORMATION ANDESITES, OKANOGAN COUNTY, WASHINGTON: UNIVERSITY OF WASHINGTON MASTER OF SCIENCE THESIS, 26 P., 1 PL.

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): 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): LANDES, HENRY; THYNG, W.S.; LYON, D.A.; ROBERTS, MILNOR, 1902, ANNUAL REPORT FOR 1901, IN SIX PARTS; PART-II THE METALLIFEROUS RESOURCES OF WASHINGTON, EXCEPT IRON: WASHINGTON GEOLOGICAL SURVEY, 123 P.

Reference (Deposit): WASHINGTON DIVISION OF MINES AND MINING, 1941, DIRECTORY OF WASHINGTON MINING PROPERTIES: WASHINGTON DIVISION OF MINES AND MINING INFORMATION CIRCULAR 7, 74 P.


Washington Gold

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