The Mikado Mine is a gold mine located in Alaska.
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
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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.
Mikado Mine MRDS details
Site Name
Primary: Mikado Mine
Secondary: Carter
Secondary: Crystal
Secondary: Eclipse
Secondary: Engineers Exploration Syndicate
Secondary: Golden Eagle
Secondary: Idaho-Alaska Corp.
Secondary: Little Mikado
Secondary: Overlook
Secondary: Tobin
Commodity
Primary: Gold
Secondary: Silver
Tertiary: Antimony
Tertiary: Lead
Tertiary: Zinc
Location
State: Alaska
District: Chandalar
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Producer
Operation Type: Unknown
Year Last Production: 1982
Discovery Year: 1909
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: Oxidized To 75 Ft; Principal Oxidation Products: Scorodite And Limonite
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Sphalerite
Ore: Stibnite
Ore: Galena
Gangue: Quartz
Gangue: Pyrite
Gangue: Limonite
Comments
Comment (Commodity): GEOCHEMICAL SAMPLES SHOW HIGH CONCENTRATIONS OF AG, AS, PB, SB AND ESPECIALLY ZN; CU CONTENT GENERALLY LOW
Comment (Reserve-Resource): PROVEN RESERVES IN 1979: MORE THAN 30,000 TONS GRADING 1 OZ/TON AU, ADGGS REVIEW OF ALASKA'S MINERAL RESOURCES, 1981-82, P. 20.
Comment (Deposit): NW TRENDING SHEAR ZONE ABOUT 50 FT WIDE CONTAINS SUBPARALLEL, HIGHLY FAULTED AND BRECCIATED AURIFEROUS QUARTZ VEINS UP TO 2 M THICK EXPOSED FOR OVER 900 M ALONG MIKADO FAULT; MIKADO VEIN AVERAGES 6 FT IN THICKNESS OVER 500 FT STRIKE LENGTH; MOST VEINS DISCONTINUOUS, A FEW TENS 'OR HUNDREDS OF FT LONG; VEINS CARRY VISIBLE FREE GOLD AND LESS THAN 5% SULFIDES; SULFIDES PRESENT: PYRITE, ARSENOPYRITE, SPHALERITE, GALENA AND STIBNITE
Comment (Workings): 60 M SHAFT, 140 M CROSSCUT AND OPEN CUTS, 1909-1913; WORKINGS CAVED BY 1923; MORE THAN 200 M ADDED UNDERGROUND AND SOME SURFACE TRENCHING IN 1959-1960; 260 M OF DRIFTING AND CROSSCUTTING DONE WITH OME ASSISTANCE IN 1962-63; UNKNOWN AMOUNT OF WORK DONE IN LATE 60'S, LATE 70'S AND EARLY 80'S; MILL REDESIGATED, 1981; 125 TPD
Comment (Location): ADGGS GR 42, FIGURE 2; LOCATION IS GIVEN FOR MIKADO LODE; NUMEROUS CLAIMS AND QUARTZ VEINS IN IMMEDIATE VICINITY; MOST OR POSSIBLY ALL MINING ON THE MIKADO VEIN LAND STATUS VALUE CALCULATED 6-94 USING GIS OVERLAY ANALYSIS WITH BLM 1:2,500,000 SCALE OWNERSHIP STATUS MAP (1991).
Comment (Production): REPORT ON 1983 MINING ACTIVITY IN ALASKA STATES: AN ESTIMATED 10,000 OZ AU PRODUCED "DURING THE LAST SEVERAL YEARS"; ADGGS SR 33, P. 16
Comment (Development): FIRST UNDERGROUND DEVELOPMENT, 1909-1913; MINE REOPENED BY LITTLE SQUAW MINING CO. IN 1959-1960; UNDERGROUND WORK IN 1962-1963 DONE WITH OFFICE OF MINERALS EXPLORATION (OME) ASSISTANCE; UP TO 100 TPD MILLED INTERMITTENTLY IN THE LATE 60'S TO THE EARLY 80'S; MILL REDESIGNED IN 1981 TO INCLUDE CYANIDE-LEACHING AND FLOTATION CIRCUIT, MILL CAPACITY INCREASED TO 125 TPD; MILL OPERATED FOR 38 DAYS IN 1982; WORK IN 1983 RESTRICTED TO UNDERGROUND DEVELOPMENT DRILLING AND DRIFTING; NO WORK IN 1984
Comment (Geology): GENERAL AREA IS UNDERLAIN BY DEVONIAN SCHIST AND PHYLLITE CUT BY GREENSTONE SILLS AND DIKES; THE AREA E OF CHANDALAR LAKE IS CUT BY A SERIES OF NW TRENDING FAULTS; THE CHANDALAR AREA IS PART OF A LARGE REGION THAT IS DOMINATED BY NE TRENDING FOLDS AND THRUST PLATES, LOCALLY INTRUDED BY NE TRENDING BODIES OF GRANITIC ROCK AND BORDERED ON THE S BY E-W TRENDING FOLDS AND A GRANITIC BATHOLITH ELONGATED E-W. MIKADO PHYLLITE, SUBUNIT OF DEV. SCHIST; PROMINENT INTERBED OF PHYLLITE IN QUARTZ-MUSCOVITE SCHIST
Comment (Deposit): SEE ALSO: LITTLE SQUAW, TOBIN CREEK ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT
References
Reference (Deposit): USGS PP 709, P. 3, 14-16
Reference (Deposit): ADGGS GR 42, P. 5, 19-21, FIG. 2
Reference (Deposit): USGS BULL 773, P. 262
Reference (Deposit): USGS BULL 532, P. 112-115
Reference (Deposit): USGS CIRC 758, P. 3
Reference (Deposit): USGS MF-878-B, LOC. 47
Reference (Deposit): USGS OFR 77-166-C, P. 37, LOC. 45A
Reference (Other Database): BAG-MF-878B-47
Reference (Deposit): ADGGS SR 38, P. 7, 23
Reference (Deposit): ADGGS SR 33, P. 11, 16, 23
Reference (Deposit): ADGGS, REVIEW OF ALASKA'S MINERAL RESOURCES, 1981-82, P. 19-20, 30
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