Addison

The Addison is a tungsten, copper, lead, zinc, silver, and gold mine located in Ferry 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: Addison  

State:  Washington

County:  Ferry

Elevation:

Commodity: Tungsten, Copper, Lead, Zinc, Silver, Gold

Lat, Long: 48.05056, -118.58111

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 Addison

Addison MRDS details

Site Name

Primary: Addison
Secondary: Pacific Mutual


Commodity

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


Location

State: Washington
County: Ferry


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
Years of Production:
Organization:
Significant: N


Physiography

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


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Not available


Alterations

Not available


Rocks

Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Eocene


Analytical Data

Not available


Materials

Ore: Galena
Ore: Sphalerite
Ore: Wolframite
Ore: Chalcopyrite
Ore: Malachite
Ore: Scheelite
Ore: Lead
Ore: Chalcocite
Gangue: Quartz


Comments

Comment (Development): ECON.COM: PRODUCED A SMALL AMOUNT OF LEAD, COPPER, ZINC, SILVER, AND GOLD IN 1923 (HUNTTING, 1956, P. 51). PRODUCED 1500 TONS OF ORE IN 1973 (MOEN, 1976, P. 100).

Comment (Deposit): ORDOVICIAN? SEDIMENTARY ROCKS OF THE COVADA GROUP HOST QUARTZ VEINS AT THE ADDISON MINE. THE SEDIMENTARY ROCKS ARE NEAR PALEOCENE TO EOCENE GRANODIORITE. NUMEROUS EOCENE HYPABYSSAL DIKES ARE FOUND IN THE AREA (JOSEPH, 1990, GEOL, MAP, P. 6-7). ; INFO.SRC : 1 PUB LIT


References

Reference (Deposit): WDGER OFR 90-18

Reference (Deposit): CULVER, H.E.; BROUGHTON, W.A., 1945, TUNGSTEN RESOURCES OF WASHINGTON: WASHINGTON DIVISION OF GEOLOGY BULLETIN 34, 89 P., 23 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): JOSEPH, N.L., COMPILER, 1990, GEOLOGIC MAP OF THE NESPELEM 1:100,000 QUADRANGLE, WASHINGTON: WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES OPEN FILE REPORT 90-16, 47 P., 1 PL.

Reference (Deposit): MOEN, W.S., 1976, SILVER OCCURENCES IN WASHINGTON: WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES BULLETIN 69, 188 P.


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