The Unnamed is a gold, silver, and copper 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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Unnamed MRDS details
Site Name
Primary: Unnamed
Commodity
Primary: Gold
Primary: Silver
Primary: Copper
Secondary: Zinc
Location
State: Alaska
District: Alaska Peninsula
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Model Name: Epithermal vein, generic
Orebody
Not available
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: Propylitic alteration is present to a moderate extent in the diorite and may be more common in the volcanic rocks. Hydrothermal minerals include chlorite, epidote, clay, and locally magnetite.
Rocks
Name: Volcanic Rock (Aphanitic)
Role: Host
Age Type: Host Rock
Age Young: Pliocene
Name: Volcanic Rock (Aphanitic)
Role: Host
Age Type: Associated Rock
Age Young: Pliocene
Analytical Data
Not available
Materials
Ore: Pyrite
Gangue: Magnetite
Comments
Comment (Workings): Workings / Exploration = Christie (1974) reports brief reconnaissance geologic mapping and the collection of more than 30 soil and silt samples. Copper content typically was less than 50 ppm, although one sample yielded 101 ppm. Zinc ranged as high as 490 ppm, silver to 4.1 ppm and gold to 0.03 ppm.
Comment (Geology): Geologic Description = Christie (1974) briefly examined an east-west oriented 1 by 4 mi (1.6 by 6.4 km) color anomaly. The anomaly occurs in andesitic volcanic rocks, that include flows, pyroclastic rocks and breccia intruded in the center of the anomaly by a medium-grained dioritic pluton, on the east by a feldspar porphyry and on the west by minor diorite dikes. At east end of the color anomaly, a large covered area 1 mi (1.6 km) wide of indeterminate length may expand the occurrence. Volcanic rocks contain disseminated and fracture-controlled pyrite; mineralization does not increase at contact with the diorite. Both the diorite and volcanic rocks are cross-cut by thin breccia zones composed of severely leached and bleached angular wall rocks in a matrix of iron oxide. At western end of the anomaly, pyrite concentrations are highest in pyroclastic rock and breccia units.
Comment (Deposit): Other Comments = No quartz veins are mentioned by Christie (1974), but this does not indicate that they are absent, inasmuch as his focus was mainly on porphyry mineralization.
Comment (Deposit): Model Name = Epithermal gold vein
Comment (Reference): Primary Reference = Christie, 1974
Comment (Exploration): Status = Inactive
Comment (Geology): Age = Miocene or younger
References
Reference (Deposit): MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous mineral deposits in the western part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-F, 38 p., 1 sheet, scale 1:1,000,000.
Reference (Deposit): Christie, J.S., 1974, Aleut-Quintana-Duval 1974 joint venture, final report: Unpublished Quintana Minerals Corporation report, 24 p., 3 appendices, 2 maps. (Report held by the Aleut Corporation, Anchorage, Alaska.)
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