Hoosier Creek Mine, Rampart Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
| Regional Level Types | |
|---|---|
| Hoosier Creek Mine | Mine |
| Rampart Mining District | Mining District |
| Yukon-Koyukuk Census Area | Census Area |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
65° 26' 56'' North , 150° 5' 27'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Location: The Hoosier Creek placer mine is marked by tailings, starting from about 0.5 mile from the mouth of the creek, upstream for about 2 miles (Cobb, 1972). The site is at about the midpoint of the tailings, in the northeast quarter of section 7, T. 7 N., R. 12 W., of the Fairbanks Meridian. The location is accurate. The site corresponds to location 48 of Cobb (1972), and roughly to the site for Hoosier Creek, U.S. Bureau of Land Management MAS number 0020480078.
Geology: Hoosier Creek drains an area underlain upstream by Cambrian or late Proterozoic quartzite, feldspathic quartzite, grit, calcareous siltstone, limestone, and chert (Reifenstuhl and others, 1997 [RI 97-15a]). The placer operations are underlain by Triassic(?) Rampart Group mafic and intermediate volcanic and intrusive rocks, chert, and tuff. Gold was discovered before 1902 (Mertie, 1934), and by 1904 preparations were made for hydraulicking 2 miles above the mouth of the creek (Prindle and Hess, 1905). The dimensions of the pay zone were never well defined, but averaged between 100 and 150 feet wide (Mertie, 1934). By 1928, Hoosier Creek was being drift mined, mostly during the winter, because there was not enough water or enough gradient in the stream to run the sluiceboxes during the summer (Mertie, 1934). U.S. Geological Survey reports describe mining on the stream fairly continuously through 1938 (Smith, 1939 [B 917-A]; Cobb, 1977). In 1957, Saunders (1957 [MR 194-17]) reported that the Weisner Trading Company intended to mine on Hoosier Creek, and implied that mining had occurred on the creek in the recent past. Mining or mining claims were active in 1967 (Heiner and others, 1968). Eakin and others (1985) and Bundtzen and others (1987) reported that the Hoosier Creek Mining Company was successful. In 1988, Willford Mining cleared ground, stripped overburden and constructed settling ponds in preparation for mining, and mined into 1990 (Green and others, 1989; Bundtzen and others, 1990; Swainbank and others, 1991). In 1991, Lucas Mining, and in 1992, Jimmy Dale, operated on Hoosier Creek (Bundtzen and others, 1992; Swainbank and others, 1993). Mining was reported on Hoosier and Little Hoosier creeks in 1996 (Swainbank and others, 1997), and in 1997, Frank Willford mined a tributary to Hoosier Creek (Swainbank and others, 1998). Some of the gold mined was coarse, including a $250 nugget (gold at $20.67? per ounce). The gold was about 941 fine (Mertie, 1934). The heavy minerals collected with the gold included hematite, ilmenite, barite, magnetite, pyrite, garnet, picotite, scheelite, zircon, native copper and cinnabar (Mertie, 1934; Waters, 1934). The stream gradient is 100 feet per mile. Eight gold grains, including several small nuggets and one large nugget from Hoosier Creek were analyzed by electron microprobe (Newberry and Clautice, 1997). Five of the grains had nearly identical compositions characterized by cores with fineness of 800 to 810, Cu and Hg below detection, and Bi and Te at detection levels. Two other grains had cores of higher fineness, and rims with finenesses up to 990. Most of the grain compositions are similar to those of the gold recovered from the nearby Elephant Mountain (TN067) deposit (Newberry and Clautice, 1997). Diabase bedrock in Hoosier Creek (TN063) contains auriferous quartz-pyrite veins that possibly are the source of some of the placer gold (Hess, 1908). The diabase is covered by 6 to 15 feet of alluvium. White mica from one of the veins yielded an Ar40/Ar39 age of 72.2 +/- 0.3 Ma (Reifenstuhl and others, 1997 [PDF 97-29h]).
Workings: Mining on Hoosier Creek began sometime before 1904. Both hydraulicking and drift mining techniques were used, but the stream gradient was not high enough for sluicing in midsummer (Mertie, 1934). Mining activity appears to have been continuous through 1938. Annual reports were not published by the U.S.Geological Survey after 1940 and reporting became sporadic (Cobb, 1977). Saunders (1957 [MR 194-17]) reported that the Weisner Trading Company intended to mine on Hoosier Creek in 1957 and implied that mining had occurred on the creek in the recent past. Mining or mining claims were active in 1967 (Heiner and others, 1968). Eakin and others (1985) and Bundtzen and others (1987) reported that the Hoosier Creek Mining Company successfully mined on Hoosier Creek in 1984 and 1986. In 1988, Willford Mining cleared and stripped overburden and constructed settling ponds in preparation for mining in 1990 (Green and others, 1989; Bundtzen and others, 1990; Swainbank and others, 1991). In 1991, Lucas Mining, and in 1992, Jimmy Dale, operated on Hoosier Creek (Bundtzen and others, 1992; Swainbank and others, 1993). Mining was reported on Hoosier and Little Hoosier creeks in 1996 (Swainbank and others, 1997), and in 1997, Frank Willford mined a tributary (Swainbank and others, 1998).
Age: Quaternary.
Production: By 1904, $2,000 worth of gold (at $20.67 per ounce) had been produced from Hoosier Creek (Hess, 1908). By 1931, claims 13 and 14 above Discovery produced a total of $50,000 worth of gold (at $20.67 per ounce) (Mertie, 1934). The gold was about 941 fine.
Commodities (Major) - Au; (Minor) - Cu, Hg, Pb, W
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
10 valid minerals.
Detailed Mineral List:
| ⓘ Baryte Formula: BaSO4 |
| ⓘ Cinnabar Formula: HgS |
| ⓘ Galena Formula: PbS |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Gold Formula: Au |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Scheelite Formula: Ca(WO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | Native Gold | 1.AA.05 | Au |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Cinnabar | 2.CD.15a | HgS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Scheelite | Ca(WO4) |
| S | Sulfur | |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Cinnabar | HgS |
| S | ⓘ Galena | PbS |
| S | ⓘ Pyrite | FeS2 |
| Ca | Calcium | |
| Ca | ⓘ Scheelite | Ca(WO4) |
| Ti | Titanium | |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | Iron | |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Native Copper | Cu |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| W | Tungsten | |
| W | ⓘ Scheelite | Ca(WO4) |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
| Hg | Mercury | |
| Hg | ⓘ Cinnabar | HgS |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Databases
| Link to USGS - Alaska: | TN059 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Angayucham TerraneAccretionary Complex
- Ruby DomainDomain
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