The Unnamed (Boulder Creek east bench) 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
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Unnamed (Boulder Creek east bench) MRDS details
Site Name
Primary: Unnamed (Boulder Creek east bench)
Commodity
Primary: Gold
Secondary: Tungsten
Secondary: Arsenic
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 Text: Sulfidation of schist.
Rocks
Not available
Analytical Data
Not available
Materials
Ore: Arsenopyrite
Ore: Pyrite
Ore: Scheelite
Gangue: Quartz
Comments
Comment (Exploration): Status = Inactive
Comment (Deposit): Other Comments = The northwesterly trending mineralization at this prospect may be cut off or displaced by the Rodine fault (Bundtzen and others, 1994).
Comment (Workings): Workings / Exploration = Kennecott Exporation Company completed about 900 feet of trenches in 1992 to follow up arsenic and gold soil anomalies on the bench northeast of the confluence of Twin Mountain and Boulder Creek. The trenches were backfilled and reclaimed after mapping and sampling.
Comment (Reference): Primary Reference = This report
Comment (Deposit): Model Name = Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a).
Comment (Geology): Age = Mid-Cretaceous; postdates regional metmorphism and is probably similar in age to other low-sulfide Au-quartz veins of the Nome district (see, for example, the Divide prospect, NM058).
Comment (Geology): Geologic Description = This prospect was discovered in 1992 by following up results of a soil geochemistry survey. Mineralization continues to the south and the prospect is also probably related to quartz and sulfide vein mineralization reported as the Dakota group of some 13 claims (NM174) on Boulder Creek below Twin Mountain Creek (Mertie, 1918 [B 662-I, p. 429]). A soil geochemistry survey was completed on the northeast bench of Boulder Creek downstream from its confluence with Twin Mountain Creek in 1991. Soil samples were collected on 50-foot intervals on northeast lines about 200 feet apart. Some samples contained more than 1 percent arsenic and more than 2,000 ppb gold. In general, a strong arsenic anomaly (values in hundreds of parts per million) extends northwesterly across the bench. A series of five trenches with a total length of 900 feet was excavated; four were parallel to the soil sample lines and one crossed them. All trenches found mineralized zones, although establishing continuity between individual zones was difficult. A trench excavated on the soil line with values greater than 1 percent arsenic and 2,000 ppb gold (Trench NEBLdr-T1, Kennecott Exploration Company, written communication, 1992) found a massive quartz-arsenopyrite vein below 10 feet of overburden. A 30-foot-long zone in bedrock centered on the vein averaged 6.4 ppm gold and greater than 1 percent arsenic. Trenches 80 feet west and 100 feet east found lower values; these consisted of as much as 10 feet of 1,020 ppb gold 100 feet to the east and 10 feet of 4,400 ppb gold 80 feet to the west. A trench excavated 400 feet to the west of Trench NEBLdr-T1 contained one 10-foot sample with greater than 10 ppm gold and a 30-foot sample with about 500 ppb gold. This mineralization probably extends northwesterly into Twin Mountain Creek and could include the occurrences described in two adits driven into the east side of Twin Mountain (Cathcart, 1922, p. 251). One of these adits reportedly contained scheelite in a quartz-feldspar vein. The northwesterly trending mineralization at this prospect may be cut off or displaced by the Rodine fault (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): Cathcart, S.H., 1922, Metalliferous lodes in southern Seward Peninsula: U.S. Geological Survey Bulletin 722, p. 163-261.
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