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Old No. 2 Prospect, Fairbanks Mining District, Fairbanks North Star Borough, Alaska, USAi
Regional Level Types
Old No. 2 ProspectProspect
Fairbanks Mining DistrictMining District
Fairbanks North Star BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 59' 31'' North , 147° 45' 32'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Fox417 (2011)7.6km
Farmers Loop4,853 (2017)9.7km
College12,964 (2011)15.1km
Fairbanks32,325 (2017)17.3km
Ester2,422 (2011)20.1km
Mindat Locality ID:
199240
Long-form identifier:
mindat:1:2:199240:6
GUID (UUID V4):
0


Location: This prospect is on the south side of Old Murphy Dome Road; it is across the road from the western gate to the road down to the Scrafford mine (FB077) in the NE1/4 sec. 21, T. 2 N., R. 1 W., Fairbanks Meridian.
Geology: The following geologic description is summarized from a report by Sam Dashevsky (1993) on work done by American Copper and Nickel Company on the Eagle Creek property in the early 1990's. In 1964, a high-grade antimony shear zone, the No. 2 vein, was discovered by Silver Ridge Mining Co. The shear was explored by minor trenching and a 35-foot shaft. In 1976, high gold values were recognized at the prospect. The prospect is within sub-horizontal, quartz-mica and graphitic phyllitic schists that are cut by a 4.5-foot-wide zone filled with gouge. The fault zone is exposed in one of several sloughed trenches that trend east-northeast across the ridge along Old Murphy Dome road. The fault zone is exposed for 160 feet along strike in trenches; it is 3.5 to 9.5 feet thick and extends beyond the trenches for an unknown distance. Twenty-five feet of schist in the footwall contains 220 to 750 ppb gold and averages 0.01 ouncesof gold per ton. A 4.5-foot-wide fault zone at the southeast end of the trench averages 11,300 ppb gold (0.33 ounce of gold per ton) and 1 to 3 percent antimony. A reverse circulation drill hole intercepted a weakly mineralized zone, 5 feet long of quartz, limonitic schists, and abundant gouge that contained 130 ppb gold, 722 ppm arsenic, and 1,334 ppm anitmony. Limonitic footwall schist persists for 85 feet,and is truncated by a shear zone that runs 0.06 ouncesof gold per ton over 5 feet.
Workings: In 1964, a high-grade antimony shear zone, the No. 2 vein, was discovered by Silver Ridge Mining Co. while clearing a turnout beside the road. Minor trenching took place, and a 35-foot shaft was sunk. The original trenches were periodically cleaned out and resampled by later operators. In 1991, additional prospecting was conducted by American Copper and Nickel Company and one hole was drilled.
Alteration: Pervasive iron-staining is found in the footwall schist. Clay-sericite alteration and fault gouge are developed in the shear zone (Dashevsky, 1993).

Commodities (Major) - Au, Sb
Development Status: Undetermined
Deposit Model: Gold-antimony shear zone in quartz-mica and graphitic, phyllitic schists.

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


2 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Stibnite2.DB.05Sb2S3

List of minerals for each chemical element

SSulfur
S StibniteSb2S3
SbAntimony
Sb StibniteSb2S3
AuGold
Au Native GoldAu

Other Databases

Link to USGS - Alaska:FB079

Other Regions, Features and Areas containing this locality


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