The Alpha Ridge is a 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
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.
Alpha Ridge MRDS details
Site Name
Primary: Alpha Ridge
Commodity
Primary: Gold
Secondary: Silver
Secondary: Lead
Secondary: Antimony
Secondary: Arsenic
Secondary: Zinc
Location
State: Alaska
District: Nome
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: Low-sulfide Au-quartz vein
Orebody
Not available
Structure
Not available
Alterations
Alteration Type: L
Alteration Text: Albitization associated with the introduction of arsenopyrite and other metallic minerals in schist.
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Stibnite
Ore: Sphalerite
Ore: Gold
Ore: Galena
Ore: Arsenopyrite
Gangue: Quartz
Gangue: Ankerite
Gangue: Albite
Comments
Comment (Exploration): Status = Probably inactive
Comment (Geology): Age = Mid-Cretaceous; postdates regional metmorphism and may be similar in age to low-sulfide Au-quartz veins of the Nome district (see, for example, the Divide prospect, NM058).
Comment (Deposit): Model Name = Low-sulfide Au-quartz veins ? (Cox and Singer, 1986; model 36a).
Comment (Reference): Primary Reference = This report
Comment (Workings): Workings / Exploration = About 1000 feet of trenches was excavated in 1991. An extensive soil geochemistry survey, part of a grid that extended from Monument Creek to Bangor Creek, was also completed between 1991 and 1993 by Kennecott Exploration Company. The prospect was probably originally located before 1920.
Comment (Geology): Geologic Description = The Alpha Ridge prospect is an old prospect but its location was first reported by Sainsbury and others (1972 [OFR 72-321]). It was explored by Kennecott Exploration Company from 1990 to 1993. A series of soil samples collected in a reconnaissance survey were anomalous in arsenic, gold, and other elements. The reconnaissance survey was followed up with a detailed soil geochemical survey and trenching; about 1,000 feet of trenches were excavated with a trackhoe. Mineralization at the site is associated with highly albitized, arsenic-rich rocks and with massive quartz veins; the mineralization appears to be crudely stratabound (C.C. Hawley, Cindy Buxton, and D.L. Olson, written communication, 1992). The most intense mineralization is in an area about 300 by 300 feet on the crest of the ridge immediately below a saddle at an elevation of 1,040 feet. This saddle coincides with a high-angle fault of nearly east-west strike. To the east this fault trends toward the head of the placer gold deposit on Alpha Creek (NM196) in the Nome C-1 quadrangle. Maximum gold content found in the trench samples was 2,200 ppb; numerous samples contained more than 500 ppb gold and more than 10,000 ppm arsenic. Lead and zinc are also locally strongly enriched. The highest lead and zinc contents are associated with a massive, west-northwest-striking quartz vein that is exposed in a trench and in rubble about 300 feet north of the fault-controlled saddle. Lead values in galena and possibly as an oxidized mineral, are as high as 5,000 ppm in rock samples. Zinc, inferred to originally have been in sphalerite, is as high as 580 ppm. Antimony is consistently anomalous in the trench samples. The highest antimony value, 370 ppm, coincides with a gold value of 2,900 ppb. Although the main area of mineralization is below the strong fault which underlies the saddle at the south end of the prospect, areas of albitized rock with quartz float exist at least 1,000 feet north of the area of most intense mineralization. Grab samples from outlying areas locally contain more than 9,000 ppb gold. The auriferous area on Alpha Ridge almost certainly contributed placer gold to Sledge Creek (NM169), as well as to the Alpha Creek placer (NM196) in the Nome C-1 quadrangle. The prospect is near the crest of a major antiform, and country rock is the calcareous metaturbidite schist unit of Bundtzen and others (1994).
References
Reference (Deposit): Bundtzen, T.K., Reger, R.D., Laird, G.M., Pinney, D.S., Clautice, K.H., Liss, S.A., and Cruse, G.R., 1994, Progress report on the geology and mineral resources of the Nome mining district: Alaska Division of Geological and Geophysical Surveys, Public Data-File 94-39, 21 p., 2 sheets, scale 1:63,360.
Reference (Deposit): Sainsbury, C.L., Hudson, T.L., Ewing, Rodney, and Marsh, W.R., 1972, Reconnaissance geologic map of the Nome C-2 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 72-321, 13 p., 1 sheet, scale 1:63,360.
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.
