The HOM (Mina Creek) is a zinc, silver, and lead 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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HOM (Mina Creek) MRDS details
Site Name
Primary: HOM (Mina Creek)
Commodity
Primary: Zinc
Primary: Silver
Primary: Lead
Secondary: Copper
Location
State: Alaska
District: Fairhaven
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: Massive sulfide, kuroko
Orebody
Not available
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: The deposit is oxidized; quartz-sericite-pyrite alteration is inferred to be present.
Rocks
Role: Host
Age Type: Host Rock
Age Young: Devonian
Analytical Data
Not available
Materials
Ore: Sphalerite
Ore: Galena
Ore: Chalcopyrite
Gangue: Quartz
Gangue: Pyrite
Comments
Comment (Geology): Age = Devonian ; this is a strataform deposit and the host felsic schist is interpreted to be similar in age to the Devonian gneiss at Kiwalik Mountain (Till and others, 1986).
Comment (Workings): Workings / Exploration = Some core drilling took place here in the 1970's.
Comment (Deposit): Model Name = Kuroko massive sulfide (Cox and Singer, 1986; model 28a)
Comment (Geology): Geologic Description = This is a volcanogenic massive sulfide prospect that was explored by Houston Oil and Minerals (HOM) in the 1970's. Exploration included core drilling. Drilling encountered up to 5 % sphalerite in felsic schist with some galena and silver values (R. Cunningham, written communication, 1998). The felsic schist is probably similar to other felsic schist sequences that are present in a belt to the east, south, and west of Kiwalik Mountain. The metamorphic assemblage containing felsic schist was not mapped separately by Till and others (1986) except along a part of Independence Creek. It is inferred to be of Devonian age, the age of the Kiwalik Mountain gneiss (Till and others, 1986). The geologic setting for this prospect and that at Big Bar (BN083, south of Kiwalik Mountain) seems to be similar to that of the Ambler district in the southern Brooks Range.
Comment (Reference): Primary Reference = This description
Comment (Exploration): Status = Probably inactive
References
Reference (Deposit): Till, A.B., Dumoulin, J.A., Gamble, B. ., Kaufman, D.S., and Carroll, P.I., 1986, Preliminary geologic map and fossil data, Soloman, Bendeleben, and southern Kotzebue quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 86-276, 10 p., 3 plates, scale 1:250,000.
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