The Stoney Vein is a silver, lead, copper, and 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
Elevation:
Commodity: Silver, Lead, Copper, Gold
Lat, Long: 61.91, -152.92000
Map: View on Google Maps
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Stoney Vein MRDS details
Site Name
Primary: Stoney Vein
Commodity
Primary: Silver
Primary: Lead
Primary: Copper
Primary: Gold
Secondary: Arsenic
Secondary: Antimony
Location
State: Alaska
District: Yentna
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Prospect
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Model Name: Polymetallic veins
Orebody
Not available
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: Calcite, epidote, sericite, tourmaline, quartz
Rocks
Role: Host
Age Type: Host Rock
Age Old: Late Jurassic
Analytical Data
Not available
Materials
Ore: Arsenopyrite
Ore: Copper
Ore: Stibnite
Ore: Sphalerite
Ore: Pyrrhotite
Ore: Pyrite
Ore: Gold
Ore: Galena
Ore: Chalcopyrite
Gangue: Epidote
Gangue: Tourmaline
Gangue: Siderite
Gangue: Quartz
Gangue: Graphite
Gangue: Dolomite
Gangue: Calcite
Comments
Comment (Commodity): Ore Material = Copper (native)
Comment (Deposit): Model Name = Polymetallic vein (Cox and Singer, 1986; model 22c)
Comment (Geology): Geologic Description = Part of the Yentna trend of Late Cretaceous/early Tertiary composite plutons (Tcp) described by Reed and Nelson (1980), the Mount Estelle pluton (Tme, Reed and Elliott, 1970) extends from Timber Creek on the south to the Portage Creek area in the north. At this site in the central part of the pluton, a biotite-hornblende-quartz monzonite intrudes Mesozoic marine sedimentary rocks (KJs) of the Kahiltna terrane. ? Two veins follow dilatational zones within the pluton along its west side (Cominco American Incorporated, unpublished reports, 1986-1987). The Main Stoney vein is steeply dipping structure that is mapped as more than 3 miles long, varies in measured width from 14 feet to 60 feet and has a vertical relief of at least 1000 feet. The mineralogy consists of alternating sulfide-quartz -carbonate vein material and altered intrusive material. The mineralogy consists of quartz-calcite-dolomite-siderite-tourmaline-pyrrhotite-chalcopyrite- arsenopyrite-pyrite-stibnite +/- graphite, sphalerite and galena. The North Stoney vein is a sub-parallel feature just west of the northern end of the Main Stoney vein. This vein is 35 feet at it's widest and has similar mineralogy to the Main Stoney vein. A third vein is located one mile to the west.
Comment (Exploration): Status = Inactive
Comment (Geology): Age = Possibly related to the Tertiary/Cretaneous pluton that is the host rock
Comment (Geology): Age = Host rock is Tertiary - Cretaceous.
Comment (Workings): Workings / Exploration = Exploration included prospecting, rock chip geochemical sampling, and mapping. Technical climbers were employed to map and sample the steep terrain.
Comment (Reference): Primary Reference = Reed and Elliott, 1970
References
Reference (Deposit): Reed, B.L., and Nelson, S.W., 1980, Geologic map of the Talkeetna quadrangle: U.S. Geological Survey Miscellaneous Investigations Map I-1174, scale 1:250,000.
Reference (Deposit): Reed, B.L., and Elliott, R.L., 1970, Reconnaissance geologic map, analyses of bedrock and stream sediment samples, and an aeromagnetic map of parts of the southern Alaska Range: U.S. Geological Survey Open-file Report 70-271, 24 p., 4 sheets, scale 1:250,000.
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