Mastodon Creek; Forty Two Gulch; Baker Gulch Mine, Circle Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types | |
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Mastodon Creek; Forty Two Gulch; Baker Gulch Mine | Mine |
Circle Mining District | Mining District |
Yukon-Koyukuk Census Area | Census Area |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
65° 28' 11'' North , 145° 17' 52'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
198776
Long-form identifier:
mindat:1:2:198776:1
GUID (UUID V4):
cb37fa88-bf02-44c7-b2dd-ce8add2a73bf
Mastodon Creek has produced more gold than any other creek in the Circle district and in its early history was known as the 'best creek in Alaska' (Dunham, 1898). See also Mammoth Creek, ARDF no. CI036, Independence Creek, ARDF no. CI029 and Miller Creek, ARDF no. CI039.
Location: The location is the intersection of Mastodon Creek and Baker Gulch. The placered area extends approximately 2 miles up and downstream, along Mastodon Creek. Mastodon Creek has its headwaters on the northeast flank of Mastodon Dome. It flows in a northeasterly direction for approximately 9.5 km before joining Independence Creek. Below this junction the creek is known as Mammoth Creek. The eastern headwater tributary of Mastodon Creek is known as Forty-Two Gulch. Baker Gulch, about 2.5 km downstream, is the only other tributary of Mastodon Creek.
Geology: Bedrock of the Mastodon Creek drainage is mostly the Middle Schist and Quartzite unit described by Wiltse and others (1995) as quartz-muscovite schist, porphyroblastic-albite-quartz-chlorite-muscovite schist, with lesser amounts of quartzose porphyroblastic albite-chlorite schist. Gold is in the basal 6 feet of unfrozen gravel, on bedrock, and in the top 7 feet of bedrock. Average depth to bedrock is 10 to 12 feet (Prindle, 1913, p. 63). Both the stream and bench gravels are auriferous. The paystreak is the richest in the district and is 200 feet wide and 7 to 10 feet thick. Gold is coarsest near the head of the stream and contains abundant quartz. Downstream the gold becomes more flaky, carries less quartz and shows an increase in fineness (.740 to .811 Au) (Mertie, 1938). Cassisterite is reported in concentrates (Cobb, 1973, [B 1374]). The gravel in Mastodon Creek is coarse and consists mainly of boulders with diameters of 10 to 30 cm, but some boulders are as much as 1 m across. Clasts are commonly subangular to rounded (Yeend, 1991, p. 13). Mining on Mastodon Creek has been nearly continous since gold was discovered. In the early 1900's, most operations consisted of 'shoveling in' gravel to an elevated sluicebox with wood riffles. A steam hoist and a hydraulic plant with a steam scraper were also used (Brooks, 1907). A dredge operated in 1912 to 1913, 1915, and 1918 to 1926. Hydraulic mining was the most favored method on Mastodon Creek for most of its history. In 1937, a dragline excavator began to be used. Baker Gulch was heavily prospected by trenching and panning in 1988 (Yeend, 1991). Production for Mastodon Creek through 1936 was between 96,758 and 145,137 fine ounces (Cobb, 1976, p. 43 to 45, [OFR 76-633]). The early mining operations recovered 0.1 to 0.15 ounces per cubic yard of gravel, whereas by the 1930's, 0.01 to 0.0125 ounces per cubic yard was a common yield (Yeend, 1991). Mastodon Creek produced an estimated 150,000 to 200,000 ounces of gold (Yeend, 1991). In 1987, an operation in the upper creek valley had to discontinue mining because the gold values were only 0.005 ounces per cubic yard (Yeend, 1991).
Workings: Mining on Mastodon Creek has been nearly continous since gold was discovered there in the late 1800's. In the early 1900's, most operations consisted of 'shoveling in' gravel to an elevated sluicebox with wood riffles. A steam hoist and a hydraulic plant with a steam scraper were also used (Brooks, 1907). A dredge operated in 1912 to 1913, 1915, and 1918 to 1926. Hydraulic mining was the most favored method on Mastodon Creek for most of its history. In 1937, a dragline excavator began to be used. Baker Gulch was heavily prospected by trenching and panning in 1988 (Yeend, 1991).
Production: Production for Mastodon Creek through 1936 was between 96,758 and 145,137 fine ounces (Cobb, 1976, p. 43 to 45, [OFR 76-633]). The early mining operations recovered 0.1 to 0.15 ounces per cubic yard of gravel, whereas by the 1930's, 0.01 to 0.0125 ounces per cubic yard was a common yield (Yeend, 1991). Mastodon Creek produced an estimated 150,000 to 200,000 ounces of gold (Yeend, 1991). In 1987, an operation in the upper creek valley had to discontinue mining because the gold values were only 0.005 ounces per cubic yard (Yeend, 1991).
Commodities (Major) - Au; (Minor) - Sn
Development Status: Yes; small
Deposit Model: Placer gold deposit (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
2 valid minerals.
Detailed Mineral List:
ⓘ Cassiterite Formula: SnO2 |
ⓘ Gold Formula: Au |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | 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 |
Sn | Tin | |
Sn | ⓘ Cassiterite | SnO2 |
Au | Gold | |
Au | ⓘ Gold | Au |
Other Databases
Link to USGS - Alaska: | CI037 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
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