The Ramsey-Rutherford 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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Ramsey-Rutherford Mine MRDS details
Site Name
Primary: Ramsey-Rutherford Mine
Commodity
Primary: Gold
Secondary: Silver
Tertiary: Lead
Tertiary: Copper
Tertiary: Zinc
Location
State: Alaska
District: Port Valdez
Land Status
Land ownership: State
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: Underground
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Year First Production: 1914
Year Last Production: 1935
Discovery Year: 1911
Years of Production:
Organization:
Significant: N
Deposit Size: S
Physiography
Not available
Mineral Deposit Model
Not available
Orebody
Not available
Structure
Type: R
Description: Major Foliation Strikes E, Dips Moderately N, About Parallel To Bedding
Type: L
Description: Fault Cuts Off Vein At 50 Ft Level; Fault Strikes S 80 E, Dips 80 N; Vein Shattered By Post-Mineralization Movement
Alterations
Not available
Rocks
Not available
Analytical Data
Analytical Data: 28.0 PPM AU, 170 PPM PB, 20 PPM ZN, SAMPLE 79BS011Y
Analytical Data: 15.0 PPM AG, 10.0 PPM AU, 30 PPM PB, ATOMIC ABSORPTION
Analytical Data: DATA FROM PICKTHORN M. S. THESIS, SAMPLE FROM MAIN VEIN, ADJACENT TO SHEAR: SEMIQUANTITATIVE SPECTROGRAPHIC
Materials
Ore: Gold
Ore: Chalcopyrite
Ore: Sphalerite
Ore: Galena
Gangue: Quartz
Gangue: Pyrrhotite
Gangue: Pyrite
Gangue: Calcite
Comments
Comment (Production): MINED INTERMITTENTLY BETWEEN ABOUT 1914-1917 AND BETWEEN 1921-1935;AMOUNT OF PRODUCTION UNKNOWN
Comment (Development): LOCATED 1911; DEVELOPMENT BEGAN 1912; SECOND LARGEST AU PRODUCER IN PRINCE WILLIAM SOUND REGION 1915-1917; LARGEST AU PRODUCER 1924
Comment (Deposit): QUARTZ VEINS CARRIED AU, CALCITE, PYRRHOTITE, PYRITE, CHALCOPYRITE, SPHALERITE AND GALENA IN DISCONTINUOUS BUNCHES; VEINS CONTAIN HORSES OF CRUSHED COUNTRY ROCK; VEINS UP TO 6 FT WIDE, AVE. 2.5 TO 3 FT
Comment (Commodity): AG PRESENT IN ANALYSIS, PROBABLY ALLOYED WITH AU; PYRRHOTITE IS MOST ABUNDANT SULFIDE
Comment (Location): LOCATION IS PLOTTED AS ADIT SYMBOL ON VALDEZ (A-6) QUADRANGLE; 1951, WITH LIMITED REVISIONS, 1980. LAND STATUS VALUE CALCULATED 6-94 USING GIS OVERLAY ANALYSIS WITH BLM 1:2,500,000 SCALE OWNERSHIP STATUS MAP (1991).
Comment (Workings): EXTENSIVE UNDERGROUND WORKINGS PROBABLY TOTALED MORE THAN 1500 FT BY 1915; WAS MILL ON SITE; CURRENT CONDITIONS UNKNOWN
Comment (Geology): VALDEZ GROUP GRAYWACKE AND ARGILLITE GENERALLY STRIKES E-W WITH MODERATE N DIP; ROCKS HAVE BEEN FOLDED INTO COMPRESSED E-W TRENDING FOLDS,OVERTURNED TOWARD THE S, THAT HAVE AXES WHICH PLUNGE GENTLY WESTWARD; THESE FOLDS HAVE BEEN FAULTED AND CUT BY MINERALIZED QUARTZ VEINS THAT ARE GENETICALLY RELATED TO THE WANING STAGES OF GREENSCHIST METAMORPHISM OF VALDEZ GROUP ROCKS. GRAYWACKE INTERBEDDED WITH MINOR ARGILLITE.
Comment (Deposit): ONE OF THE MAJOR AU PRODUCERS OF PRINCE WILLIAM SOUND; SEE ALSO: CLIFF MINE ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT
References
Reference (Deposit): USGS BULL 622, P. 45, 153, 159-161
Reference (Deposit): USGS BULL 783, P. 8
Reference (Deposit): USGS BULL 880-A, P. 22, 24
Reference (Deposit): USGS BULL 1246, P. 72
Reference (Deposit): USGS MF-438, LOC. 36
Reference (Deposit): PICKTHORN, WILLIAM, 1982, STABLE ISOTOPE AND FLUID INCLUSION STUDY OF THE PORT VALDEZ GOLD DISTRICT, S. AK: LOS ANGELES, CA, UCLA MASTER'S THESIS, 59 P.
Reference (Deposit): USGS OFR 80-892B, LOC. 28
Reference (Other Database): BAG-OFR-80-892B-28
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