Bear Gulch, Ruby Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types | |
---|---|
Bear Gulch | Group of Mines |
Ruby Mining District | Mining District |
Yukon-Koyukuk Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
64° 24' 28'' North , 155° 29' 26'' West
Latitude & Longitude (decimal):
Type:
Group of Mines
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Ruby | 165 (2017) | 36.9km |
Mindat Locality ID:
196414
Long-form identifier:
mindat:1:2:196414:4
GUID (UUID V4):
0aa13a94-b789-43f0-a02a-ef229272a1e0
Other/historical names associated with this locality:
Bear Pup Mines
Location: Bear Gulch is a 3-mile-long southwest-flowing tributary of Long Creek. Its confluence with Long Creek is near the town of Long. The coordinates given correspond to location 12 of Cobb (1972[MF405]), and mark the center of placer tailings marked on the USGS Ruby (B-5) Quadrangle map (1952, minor revisions in 1973), in section 32, T. 12 S., R. 17 E. of the Kateel River meridian. The location is accurate.
Geology: The Bear Creek basin drains off of three separate rock units, and flows on or very near to a reverse fault contact between two distinct rock units of the Tozitna terrane. Puchner and others (1998) mapped intermediate to mafic intrusive rocks, including gabbros and diorites, on the eastern side of the valley. The western side consists of interbedded phyllites, schists, meta-graywackes, greenstones and marbles. The closest granitic bodies lie 6 miles (ca. 10 km) away, toward the northeast and southeast. Gold was first discovered on Bear Gulch in 1910 (Maddren, 1912). There are two pay streaks in Bear Gulch. The main one is in a low terrace southeast of the creek. The other is at a higher level and is less rich in gold (Eberlein and others, 1977). Cassiterite and silver accompanied the gold (Mertie, 1936). The stream gravels were mined by open-cut methods until about 1933. The main pay streak was 20 to 30 feet (ca. 9 m) deep and up to 100 feet (ca. 30 m) wide, with 6 to 8 feet (2.44 m) of gold-bearing gravel (Mertie, 1936). The two most productive claims produced a total of 24,000 to 29,000 ounces (1.1 ton) of gold between 1914 and 1933 with an average composition of nuggets being 857 parts Au per thousand and 135 parts Ag per thousand (Mertie, 1936). The gold was worn but not well-rounded, and included several nuggets weighing between 2 1/2 and 100 ounces (3.78 kg) apiece (Eberlein and others, 1977).
Workings: Gold was first discovered on Bear Gulch in 1910 (Maddren, 1912). There are two pay streaks in Bear Gulch: in a low terrace southeast of the creek, and at a higher level where gold grades are lower (Eberlein and others, 1977). The stream gravels were mined by open-cut methods until about 1933 (Mertie, 1936).
Age: Quaternary.
Production: The two most productive claims along Bear Creek produced a total of 24,000 to 29,000 ounces (1.1 t) of gold between 1914 and 1933 (Eberlein and others, 1977).
Commodities (Major): - Au; (Minor) - Ag, Sn
Development Status: Yes; small
Deposit Model: Placer Au (Cox and Singer, 1986; model 39a).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
3 valid minerals.
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Silver | 1.AA.05 | Ag |
ⓘ | Gold | 1.AA.05 | Au |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Cassiterite | 4.DB.05 | SnO2 |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | ⓘ Cassiterite | SnO2 |
Ag | Silver | |
Ag | ⓘ Silver | Ag |
Sn | Tin | |
Sn | ⓘ Cassiterite | SnO2 |
Au | Gold | |
Au | ⓘ Gold | Au |
Other Databases
Link to USGS - Alaska: | RB023 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Ruby DomainDomain
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