The Goldstream is a silver 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
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Goldstream MRDS details
Site Name
Primary: Goldstream
Secondary: Bell
Secondary: Miller (and Phillips)
Secondary: Goldstone
Secondary: Goldstring
Commodity
Primary: Silver
Primary: Gold
Secondary: Copper
Secondary: Zinc
Secondary: Lead
Location
State: Alaska
District: Ketchikan
Land Status
Not available
Holdings
Not available
Workings
Not available
Ownership
Not available
Production
Not available
Deposit
Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant:
Physiography
Not available
Mineral Deposit Model
Model Name: Polymetallic veins
Model Name: Massive sulfide, Besshi (Japanese deposits)
Orebody
Not available
Structure
Not available
Alterations
Not available
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Sphalerite
Ore: Pyrite
Ore: Gold
Ore: Galena
Ore: Chalcopyrite
Ore: Arsenopyrite
Gangue: Quartz
Gangue: Calcite
Comments
Comment (Geology): Age = Late Jurassic (stratiform sulfides); Late Cretaceous or younger (quartz fissure veins).
Comment (Deposit): Other Comments = the Goldstream mine was the most productive of the early mines in the Ketchikan area. In some early reports, the property was also referred to as Bell, or Miller (and Phillips) (Brooks, 1902, p. 62; Cobb and Elliott, 1980, p. 47, 145). In 1925, two of the Goldstream claims, the Goldstone and Goldstring, were patented (Maas and others, 1995, p. 194).
Comment (Deposit): Model Name = Besshi massive sulfide?; Polymetallic veins (Cox and Singer, 1986; models 24b, 24c)
Comment (Deposit): Model Number = 24b?, 22c
Comment (Geology): Geologic Description = The country rocks on southeastern Gravina Island are Upper Jurassic or Cretaceous marine andesitic or basaltic volcanic rocks interbedded with subordinate flyschlike sedimentary rocks (Berg, 1973; Berg and others, 1988). These strata were regionally metamorphosed to greenschist-grade phyllite and semischist in Late Cretaceous time. The country rocks are cut by a high-angle fault along Tongass Narrows that displays about 4 miles of right-lateral offset.? Wright and Wright (1908, p. 177-178) describe two types of lode deposits at the Goldstream mine. The main deposit consists of apparently stratiform massive sulfides in two or more layers of greenschist or quartz-sericite schist that strike NW and dip NE, and which are separated by layers of relatively barren schist. The sulfide-rich layers in the main deposit are 4-8 feet thick and have been traced on the surface and in underground workings for 1000 feet or more. Zones of lower-grade ore are as much as 40 feet thick and several hundred feet long. The principal ore minerals in the stratiform deposits are pyrite, chalcopyrite, galena, arsenopyrite, and native gold, small particles of which accompany the sulfides and also occur in quartz seams. The other type of deposit consists of quartz-calcite fissure veins that carry galena and sphalerite, and which crosscut the massive-sulfide-bearing layers. Both types of deposits are cut by barren quartz stringers and by an altered diabase dike several feet wide that strikes N10W and dips 75NE. Several thousand tons of ore were produced in the early 1900s from the Goldstream mine, mainly from a 5-foot-long, steeply-pitching oreshoot in the main deposit (Cobb and Elliott, 1980, p. 47). Maas and others (1995, p. 201) report cumulative production of 8.1 kg Au and 15 kg Ag.? Maas and others (1995, p. 197) report that a 4-foot sample across quartz lenses in talc schist contained 4.7 ppm Au, 74.4 ppm Ag, 0.8% Cu, and 6.28% Zn. ? Maas and others (1995, p. 201) suggest that the massive-sulfide-bearing layers are of stratiform volcanogenic origin. If so, the Goldstream deposit probably can be classified as a metamorphosed Besshi massive sulfide deposit, possibly of Late Jurassic age. The sulfide-bearing quartz fissure veins that cut the stratiform deposits probably formed by remobilization, during or following Upper Cretaceous regional metamorphism.
Comment (Workings): Workings / Exploration = The Goldstream deposit was discovered in 1897 and worked mainly in the early 1900s. Some gold was also produced by reworking dump material in the 1930s. Development of the main deposit in the early 1900s included a 115-foot shaft with 2 levels (50 and 100 feet deep), and between 400 and 600 feet of drifts. The veins were developed at that time by two 50-foot shafts, opencuts, and trenches. Maas and others (1995) report that the two 50-foot shafts are plugged.? Maas and others (1995, p. 197) report that a 4-foot sample across quartz lenses in talc schist contained 4.7 ppm Au, 74.4 ppm Ag, 0.8% Cu, and 6.28% Zn.
Comment (Production): Production Notes = Several thousand tons of ore were produced in the early 1900s from the Goldstream mine, mainly from a 5-foot-long, steeply-pitching oreshoot in the main deposit (Cobb and Elliott, 1980, p. 47). Maas and others (1995, p. 201) report cumulative production of 8.1 kg Au and 15 kg Ag.
Comment (Reference): Primary Reference = Wright and Wright, 1908; Maas and others, 1995
References
Reference (Deposit): Maas, K.M., Bittenbender, P E., and Still, J.C., 1995, Mineral investigations in the Ketchikan mining district, southeastern Alaska: U.S. Bureau of Mines Open-File Report 11-95, 606 p.
Reference (Deposit): Berg, H.C., Elliott, R.L., and Koch, R.D., 1988, Geologic map of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Mineral Investigations Series Map MF-1807,27 p., scale 1:250,000.
Reference (Deposit): Cobb, E.H., and Elliott, R.L., 1980, Summaries of data on and lists of references to metallic and selected nonmetallic mineral deposits in the Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-File Report 80-1053, 154 p.
Reference (Deposit): Wright, F.E., and Wright, C.W., 1908, The Ketchikan and Wrangell mining districts, Alaska: U.S. Geological Survey Bulletin 347, 210 p.
Reference (Deposit): Berg, H.C., 1973, Geology of Gravina Island Alaska: U.S. Geological Survey Bulletin 1373, 41 p.
Reference (Deposit): Elliott, R.L., Berg, H.C., and Karl, Susan, 1978, map and table describing metalliferous and selected nonmetalliferous mineral deposits, Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-file Report, 78-73-B,17 p., scale 1:250,000.
Reference (Deposit): Brooks, A.H., 1902, Preliminary report on the Ketchikan mining district, Alaska, with an introductory sketch of the geology of southeastern Alaska: U.S. Geological Survey Professional Paper 1, 120 p.
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