Glen Gulch; Glenn Gulch Mine, Ruby Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
| Regional Level Types | |
|---|---|
| Glen Gulch; Glenn Gulch Mine | Mine |
| Ruby Mining District | Mining District |
| Yukon-Koyukuk Census Area | Census Area |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
64° 24' 58'' North , 155° 22' 58'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Ruby | 165 (2017) | 36.3km |
Location: Glen Gulch was mined along its entire length of about 2 1/2 miles. The stream is an east-flowing tributary of Flint Creek. The coordinates correspond to location 16 of Cobb (1972 [MF-405]), and mark the approximate midpoint of the creek, in section 25, T. 12 S., R. 17 E of the Kateel River meridian. The location is accurate.
Geology: The bedrock underlying Glen Gulch is Paleozoic phyllite and quartzite (Puchner and others, 1998). A small Tertiary granitic body lies about 3 1/2 miles south of its head. Gold was first discovered in Glen Gulch in 1911 (Maddren, 1912). Brooks (1915) reported that considerable drift mining was taking place in 1914. Mertie and Harrington (1916) reported that exploration drill holes, some 40 feet to bedrock, were used for prospecting in the area around this time. Mertie and Harrington (1924) reported that no extensive operations had operated since 1915, and Eberlein and others (1977) speculated that Glen Gulch was mined out soon after 1915. However, Jim Johnson (oral communication, 2000) reported that the area was mined intensively around 1915, but mining took place intermittently from 1915 until about 1985. Gravels overlying about 50,000 square feet of bedrock were mined in 1986 or 1987 yielding roughly 250 ounces of gold (Pete Haggland, oral communication, 2000). During this operation, Haggland reported that 37 drift holes were encountered. Gold was found in the bottom foot of gravel and in shattered bedrock (Mertie and Harrington, 1916). Some gold is rough and coarse, and some nuggets were valued at $150 (gold at $20.67 per ounce). There were profitable gravels along the entire creek although the pay was spotty (Eberlein and others, 1977). Near the head, the gravel was 10 to 15 feet deep and unfrozen (Eakin, 1914 [B578]). Farther downstream, gravels were 25 feet deep and frozen. Some open-cut mining took place upstream (Mertie and Harrington, 1916). The gravels near the mouth of the creek were prospected but not mined due to the frozen nature of the ground (Mertie and Harrington, 1916).
Workings: Between 1911 and 1915, mining took place near the head of Glen Gulch by open-cut methods (Mertie and Harrington, 1916). Exploration drill holes were sunk 40 feet to bedrock further downstream and some drift mining also took place during this time (Mertie and Harrington, 1916). The area was probably mined intensively around 1915, but mining took place intermittently from 1915 until about 1985 (Jim Johnson, oral communication, 2000). Gravels overlying about 50,000 square feet of bedrock were mined in 1986 or 1987, intersecting 37 drift holes and yielding roughly 250 ounces of gold (Pete Haggland, oral communication, 2000).
Age: Quaternary.
Production: In 1986 or 1987, about 250 ounces of gold were removed from gravel covering 50,000 square feet of bedrock (P. Haggland, oral communication, 2000).
Commodities (Major) - Au
Development Status: Yes
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
1 valid mineral.
Gallery:
Other Databases
| Link to USGS - Alaska: | RB030 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Ruby DomainDomain
- Ruby TerraneAccretionary Complex
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