Shellabarger Pass

The Shellabarger Pass is a zinc, lead, copper, barium-barite, gold, and silver 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

Satelite View

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.

Site Name

Primary: Shellabarger Pass
Secondary: Shellebarger Pass

Commodity

Primary: Zinc
Primary: Lead
Primary: Copper
Primary: Barium-Barite
Primary: Gold
Primary: Silver

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: Massive sulfide, Besshi (Japanese deposits)

Orebody

Not available

Structure

Not available

Alterations

Alteration Type: L
Alteration Text: Hydrothermal alteration (mineralogy unspecified) is extensive in the footwall but is rare to absent in hanging wall (Reed and Eberlein, 1972).

Rocks

Not available

Analytical Data

Not available

Materials

Ore: Galena
Ore: Sphalerite
Ore: Pyrrhotite
Ore: Barite
Ore: Chalcopyrite
Ore: Pyrite
Ore: Marcasite
Gangue: Dolomite
Gangue: Siderite
Gangue: Quartz
Gangue: Calcite

Comments

Comment (Exploration): Status = Inactive

Comment (Geology): Age = Triassic or Jurassic (Nokleberg and others, 1987, p. 48; Nokleberg and others,1994, p. 877) or latest Devonian-earliest Mississippian (Reed and Nelson, 1980).

Comment (Geology): Geologic Description = Several massive sulfide bodies lie within 1/2 mile radius of this location. According to Reed and Eberlein (1972), the Shellabarger Pass volcanogenic massive sulfide (VMS) deposits are comprised of at least six individual bodies. The massive sulfide bodies are lenticular deposits with exposed dimensions on the order of 50 to 100 feet by 17 to 27 feet, composed of 60% sulfides in a very fine grained mixture of pyrite, marcasite, sphalerite, chalcopyrite, galena and pyrrhotite. Sphalerite, chalcopyrite and galena make up about 15% of total sulfides. Some areas of heavily disseminated sulfides are localized along shear zones. Sulfide minerals are intergrown with the gangue minerals siderite, calcite, quartz, and dolomite. Sulfides and gangue occur in massive, lenticular sulfide bodies, as replacements of carbonate-rich beds, and as fracture fillings, mainly in chert and siltstone. Main sulfide bodies may be proximal to basaltic flow fronts. Regionally the basalt has high background copper values of 200 to 300 ppm. ? the grade of the massive bodies averages 1 to 1.5% copper, 0.8 to 1.7% zinc, 0.9 to 2.4 oz/ton silver and less than 0.5% lead. Gold content varies from 0.0006 to 0.15 oz/ton. The sulfide bodies tend to be zoned, with highest chalcopyrite concentrations in basal parts and minor sphalerite in or near hanging walls (Reed and Eberlein, 1972; Nokleberg and others, 1994). ? Hydrothermal alteration is extensive in the footwall but is rare to absent in hanging wall (Reed and Eberlein, 1972).? Indicated tonnage of known bodies is on the order of 50,000 tonnes (Reed and Eberlein, 1972). Nokleberg and others (1994) report an estimated several hundred thousand tonnes of unknown grade.? the host rocks are interpreted to be part of the Mystic terrane, a displaced fragment of the late Paleozoic and early Mesozoic North American Cordillera continental margin (Reed and Nelson, 1980; Decker and others, 1994; Nokleberg and others, 1994). The deposits occur in a north-trending structural trough of Triassic to Jurassic marine sediments and mafic volcanics (hypersthene normative tholeiites that includes pillow basalt, agglomerate, and breccia) in a eugeoclinal sequence which rests unconformably over Paleozoic sedimentary rocks consisting of interbedded chert, dolomite, siltstone, shale, volcanic graywacke, and basaltic aquagene tuff (Bundtzen and Gilbert, 1983; Reed and Nelson, 1980). ? It is unclear whether the deposits are hosted in Paleozoic or Mesozoic rocks. There is evidence to suggest the volcanic host rocks are either upper Triassic (Norian?) or latest Devonian-earliest Mississippian. Bundtzen and Gilbert (1983) suggest that the host rocks to the Shellabarger VMS deposits could be Late Triassic. Bundtzen and others (1997) report Late Triassic fossils in from a sedimentary/basalt sequence in the Mystic terrane to the north and east in the adjacent McGrath quadrangle. Reed and Nelson (1980) consider the basalts to be post-Late Devonian age (possibly Mississippian), indicated by distinctive spherical concretions of fluoroapatite present in sedimentary breccia and conglomerate that apparently underly the pillow basalt at Shellabarger Pass. The source of the concretions is considered to be a phosphatic chert unit that overlies the Middle and Upper Devonian limestone. A nearby pillow basalt occurs in a chaotic sequence of sedimentary rocks that contains fossils of late Middle Devonian(?) (Reed and Nelson, 1980).

Comment (Reserve-Resource): Reserves = Indicated tonnage of known bodies is on the order of 50,000 tonnes (Reed and Eberlein, 1972). Nokleberg and others (1994) report an estimated several hundred thousand tonnes of unknown grade.

Comment (Deposit): Model Name = Besshi massive sulfide (Cox and Singer, 1986; model 24b).

Comment (Deposit): Other Comments = In the past over 300 mining claims have been held in this area.

Comment (Workings): Workings / Exploration = Reconnaissance mapping, stream silt and rock sampling are all that has been published on this property. Private concerns have held the property at various times in the past and may have completed a more detailed evaluation, the results of which are not publicly available.

Comment (Reference): Primary Reference = Reed and Eberlein, 1972

References

Reference (Deposit): Clark, A.L., and Cobb, E.H., 1972, Metallic mineral resources map of the Talkeetna quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-369, 1 sheet, scale 1:250,000.

Reference (Deposit): Nokleberg, W.J., Bundtzen, T.K., Berg, H.C., Brew, D.A., Grybeck, D.J., Robinson, M.S., Smith, T.E., and Yeend, W., 1987, Significant metalliferous lode deposits and placer districts of Alaska: U.S. Geological Survey Bulletin 1786, 104 p.

Reference (Deposit): Bundtzen, T.K., Harris, E.E., and Gilbert, W.G., 1997, Geologic Map of the eastern McGrath quadrangle, Alaska: Alaska Division of Geological and Geophysical Surveys Report of Investigations 97-14, 34 pages, one sheet, scale 1:125,000.

Reference (Deposit): Nokleberg, W.J., and others, 1994, Metallogeny and major mineral deposits of Alaska and Metallogenic map of significant metalliferous lode deposits and placer districts of Alaska, in Plafker, G. and Berg, H.C., eds., The Geology of Alaska: Boulder, Colorado, Geological Society of America: The Geology of North America, v. G1, p. 855-904 and v. G1, Plate 11, scale 1:2,500,000.

Reference (Deposit): Bundtzen, T.K., and Gilbert, W.G., 1983, Outline of geology and mineral resource of upper Kuskokwim region, Alaska: Alaska Geological Society 1982 Symposium on Western Alaska, v. 3, p. 101-117.

Reference (Deposit): Decker, J., Bergman, S.C., Blodgett, R.B., Box, S.E., Bundtzen, T.K., Clough, J.G., Coonrad, W.L., Gilbert, W.G., Miller, M.L., Murphy, J.M., Robinson, M.S., and Wallace, W.K., 1994, Geology of southwestern Alaska, in Plafker, G. and Berg, H.C., eds., The Geology of Alaska: Boulder, Colorado, Geological Society of America, The Geology of North America, v. G-1, p. 285-310.

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): Cobb, E.H., and Reed, B.L., 1980, Summaries of data and lists of reference to metallic and selected nonmetallic mineral deposits in the Talkeetna quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-884, 106 p.

Reference (Deposit): Reed, B.L. and Eberlein, G.D., 1972, Massive sulfide deposits near Shellabarger Pass, southern Alaska Range, Alaska: U.S. Geological Survey Bulletin 1342, 43 p.

Reference (Deposit): MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous and selected non-metalliferous mineral deposits in the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-A, 99 p., 1 sheet, scale 1:1,000,000.

Reference (Deposit): C.C. Hawley and Associates, Inc., 1978, Mineral appraisal of lands adjacent to Mt. McKinley National Park, Alaska: U.S. Bureau of Mines Open-File Report 24-78, 275 p., 7 plates.

Reference (Deposit): Reed, B.L., Nelson, S.W., Curtin, G.C., and Singer, D.A., 1978, Mineral resources map of the Talkeetna Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-870-D, 1 sheet, scale 1:250,000.

The Top Ten Gold Producing States

These ten states contributed the most to the gold production that built the West from 1848 through the 1930s. The Top Ten Gold Producing States.