The Fuller Property is a iron mine located in Okanogan county, Washington at an elevation of 2,300 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
Elevation: 2,300 Feet (701 Meters)
Commodity: Iron
Lat, Long: 48.07028, -119.91306
Map: View on Google Maps
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Fuller Property MRDS details
Site Name
Primary: Fuller Property
Secondary: Lone Pine Claims
Commodity
Primary: Iron
Tertiary: Sulfur
Tertiary: Titanium, Metal
Tertiary: Copper
Tertiary: Phosphorus-Phosphates
Location
State: Washington
County: Okanogan
District: Squaw Creek District
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Owner Name: Fuller, A. D. (Estate)
Years: 1949 -
Owner Name: S. J. Holden
Home Office: Cle Elum, Wa.
Production
Year: 1944
Material type: ORE FE
Description: Ap_Grade: ^About 25 % Fe/Ton (Minimum) To 50 % Fe/Ton
Year: 1943
Material type: ORE FE
Description: Ap_Grade: ^Probably A Minimum Of About 25 % Fe/Ton
Year: 1942
Time Period: To 1942
Material type: ORE FE
Description: Cp_Grade: ^About 50 % Fe/Ton.
Deposit
Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year Last Production: 1944
Discovery Method: Ore-Mineral In Place
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
Form: LEDGE
Structure
Type: L
Description: Actinolite Body Contains Ore Hornblende, Biotite
Alterations
Not available
Rocks
Name: Gneiss
Role: Associated
Age Type: Associated Rock Unit
Age Young: Holocene
Name: Gneiss
Role: Associated
Age Type: Host Rock Unit
Age Young: Holocene
Name: Gneiss
Role: Associated
Age Type: Associated Rock
Age Young: Holocene
Analytical Data
Analytical Data: GOOD ORE-57.02% FE, 4.51% SIO2, .05% P2 O5, .097% S, 3.25% TIO2 2 CHANNEL SAMPLES-40.50-24.29% FE, 4.19-3.10% TIO2, .026-.024% P, .038-.004% S, .02-.11% CU
Materials
Ore: Chalcopyrite
Ore: Magnetite
Gangue: Hornblende
Gangue: Biotite
Gangue: Epidote
Gangue: Actinolite
Gangue: Quartz
Gangue: Calcite
Comments
Comment (Development): ADITS AND A QUARRY.
Comment (Commodity): 1000 TONS PRE-1943, 1250 TONS 1943, 1 CARLOAD 1944
Comment (Reserve-Resource): SHEDD AND OTHERS, 1922
Comment (Deposit): MAGNETITE INTIMATELY INTERMIXED WITH HBLENDE AND ACTINOLITE; THE ORE IS COARSE GRAINED AND HAS A SCHISTOSE (APPARENT) APPEARANCE; IT OCCURS IN SEAMS AND LENSES; THE ORE SOMEWHAT GRADES INTO THE WALL ROCK; SULFIDES ARE ASSOC. WITH QUARTZ.
Comment (Workings): 140 FT OF ADITS AND A QUARRY.
Comment (Geology): GEOL.DESC: SULFIDES ASSOCIATED WITH QUARTZ
Comment (Deposit): TWO CLAIMS: LONE PINE NOS. 1 AND 2.
References
Reference (Deposit): WASH. DMG BULL. 37, PART II, P. 198.
Reference (Deposit): WASH. DIV. GEOL. BULL 27, P. 67-69, PLATE 1
Washington Gold
"Where to Find Gold in Washington" looks at the density of modern placer mining claims along with historical gold mining locations and mining district descriptions to determine areas of high gold discovery potential in Arizona. Read more: Where to Find Gold in Washington.