The Arlington is a silver mine located in Okanogan county, Washington at an elevation of 4,081 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: 4,081 Feet (1,244 Meters)
Commodity: Silver
Lat, Long: 48.47111, -119.73167
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Arlington MRDS details
Site Name
Primary: Arlington
Commodity
Primary: Silver
Secondary: Copper
Secondary: Lead
Secondary: Gold
Tertiary: Zinc
Location
State: Washington
County: Okanogan
District: Conconcully District; Ruby Hill Area
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
Type: Unknown
Ownership
Owner Name: Arlington Mines Inc.
Years: 1937 - 1945
Production
Year: 1940
Time Period: 1888 To 1940
Material type: ORE AG AU
Description: Cp_Grade: ^ 0.02 Ozs Au
Year: 1940
Time Period: 1937 To 1940
Material type: ORE AG AU
Description: Cp_Grade: ^ 1.15 % Cu
Year: 1921
Time Period: 1916 To 1921
Material type: ORE AG AU
Description: Cp_Grade: ^Per Ton Avg: 66.6 Ozs Ag
Deposit
Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Discovery Year: 1887
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: PINCH AND SWELL
Structure
Type: R
Description: Metamorphics Structurally Trend Generally Nw.
Type: L
Description: Small Fault Offsets North Segment Of Deposit; Trans Verse Faults Offset Parts Of The Vein As Much As 10 Ft; Fault S Paralleling The Veins Have Drawn The Ore Minerals Out Into Thin Dark Gray Bands.
Alterations
Not available
Rocks
Name: Diorite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Late Cretaceous
Name: Diorite
Role: Associated
Age Type: Host Rock
Age Young: Paleocene
Name: Diorite
Role: Associated
Age Type: Host Rock Unit
Age Young: Paleocene
Name: Diorite
Role: Associated
Age Type: Associated Rock
Age Young: Late Cretaceous
Analytical Data
Analytical Data: 66 OZ AG, .02 OZ AU, 1.15% CU/TON
Materials
Ore: Pyrite
Ore: Tetrahedrite
Ore: Chalcopyrite
Ore: Galena
Ore: Sphalerite
Gangue: Quartz
Gangue: Sericite
Comments
Comment (Workings): THE WORKINGS EXPOSE THE VEIN ON 4 LEVELS. THE MAIN HAULAGE ADIT IS 1290 FT LONG AND INTERSECTS THE VEIN 972 FT F ROM THE ADIT PORTAL AND 440 FT BENEATH THE OUTCROP OF THE VEI N. FROM THE POINT WHERE THE ADIT INTERSECTS THE VEIN, OVERHEA D STOPES EXTEND 400 FT NO. AND 200 FT SO. WHERE THE ADIT INTE RSECTS THE VEIN, A WINZE HAS BEEN SUNK 100 FT. AT 50 & 100 F T BELOW THE WINZE COLLAR TWO WORKING LEVELS HAVE BEEN DEVELOP ED. THE UPPER ADIT, WHICH IS 200 FT ABOVE THE MAIN ADIT, INTE RSECTS THE VEIN 420 FT FROM THE ADIT PORTAL, & 200 FT BENEATH THE OUTCROP OF THE VEIN. THE ADIT CONTAINS OVER 700 FT OF DRI FTS AND A SHAFT THAT EXTENDS TO THE SURFACE. THE SHAFT CONTAI NS SEVERAL WORKING LEVELS FROM WHICH THE ORE HAS BEEN MINED.
Comment (Deposit): 9 PATENTED CLAIMS: ARLINGTON, ARLINGTON FR., 1806, MINNESOTA, MISSING LINK, POMEROY, PRINCESS, RILEY, EUREKA; AN D 3 UNPATENTED CLAIMS.
Comment (Commodity): PRODUCTION FROM 1888 TO 1940; HUNTING, 1956 REPORTS THAT THE 100 FT LEVEL OF THE WINZE IN THE MAIN ADIT CONTAINS 2 ORE SHOOTS THAT TOTAL 350 FT IN LENGTH, AVERGE 2.5 FT THICK , AND CONTAIN 18 OZS AG PER TON.
Comment (Reserve-Resource): WASH. DMG BULL 37, P. 300
Comment (Development): SHALLOW SHAFTS, SHORT CROSSCUTS, STOPES, AND RAISESA L45 1940
Comment (Deposit): QUARTZ VEIN AVERAGE 4-5 FT IN WIDTH WITH ORE IN BANDED SEGREGATIONS; SIMILAR PARALLEL VEINS.
Comment (Geology): THE SIMILKAMEEN BATHOLITH IS COMPOSED OF HORNBLENDE GRANODIORITE, BIOTITE GRANODIORITE, PORPHYRITIC GRANODIORITE , QTZ DIORITE, AND QTZ MONZ NITE. THE SCHISTS & GNEISSES WERE DERIVED FROM PALEOZOIC SEDIMENTS & VOLCANICS THAT WERE REGIO NALLY METAMORPHOSED DURING A JURASSIC OROGENY. ELSEWHERE IN T HE DISTRICT THE PREDOMINANT ROCKS ARE TRIASSIC LIMESTONE, MAR BLE, & DOLOMITE, & PRE-TERTIARY QTZITE, METAGRAYWACKE, AMPHIB OLITE, GREENSTONE, AND METAVOLCANICS. ; GEOL.DESC: QUARTZ FISSURE VEIN
References
Reference (Deposit): WASH. DMG BULL. 378 P.300
Reference (Deposit): WASH. GEOL. SUR. BULL 23, P. 250-253
Reference (Deposit): WASH. DGER BULL 69, P. 106-110
Reference (Deposit): WASH. DMG IC 49, P. 10-13
Reference (Production): WASH. GEOL. SUR. BULL 23, P. 251; WASH. DMG BULL 37 , P. 300; WASH. DGER BULL 69, P. 108
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.