Six Gulch Mine (Last Chance Gulch), Innoko Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
| Regional Level Types | |
|---|---|
| Six Gulch Mine (Last Chance Gulch) | Mine |
| Innoko Mining District | Mining District |
| Yukon-Koyukuk Census Area | Census Area |
| Alaska | State |
| USA | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
62° 57' 54'' North , 156° 30' 43'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Location: Six Gulch, formerly known as Last Chance Gulch is a west and northwest flowing tributary of Ganes Creek (Maddren, 1910). The mine extends up Six Gulch for about 800 feet. The coordinates are at the mouth of gulch in the SE1/4 NE1/4, section 8, T. 33 N., R. 38 W., of the Seward Meridian. The location is accurate. Cobb (1972 [MF 363]; 1976 [OFR 76-576]) referred to the site as Last Chance Gulch and described it as locality 42.
Geology: Six Gulch is a 2-mile-long tributary of Ganes Creek (ID011). It is locally incised into detrital sedimentary rocks of the Upper Cretaceous, Kuskokwim Group, which are intruded by Cretaceous or Tertiary, felsic to mafic dikes and sills (Bundtzen and Laird, 1982; Miller and Bundtzen, 1994) Placer gold, locally accompanied by scheelite, was probably derived from mineralized dikes and sills. Stream gravels consist of locally derived sandstone, siltstone, and shale from the Kuskokwim group, and intrusive rocks (Bundtzen and Laird, 1982; Miller, Bundtzen, and Gray, 2005). Gold was discovered on Ganes Creek in 1906 at the mouth of Six Gulch, then called Last Chance Creek (Maddren, 1910). The Six Gulch placer was mined for about 800 feet above its mouth. Early production was from open cuts; however, a dredge operated at the mouth of Six Gulch during the early 1930s (Mertie, 1936).
Workings: Prospectors following up the occurrences flour gold on the Innoko River and lower Ganes Creek found an economic placer deposit at the mouth of Six Gulch in 1906. The deposit was worked on a small scale for about 20 years and was dredged in the 1930s.
Age: Quaternary; probably mid-to-late Pleistocene (Bundtzen, 1980 [MIRL]).
Production: Six Gulch has produced gold for many years. The production is probably aggregated with Ganes Creek (ID011).
Reserves: There are possible gold resources in upper Six Gulch and at the sides of paystreaks that have been mined.
Commodities (Major) - Au; (Minor) - Ag, W
Development Status: Yes: small
Deposit Model: Placer Au 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:
| ⓘ Native Gold Formula: Au |
| ⓘ Scheelite Formula: Ca(WO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Gold | 1.AA.05 | Au |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Scheelite | 7.GA.05 | Ca(WO4) |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Scheelite | Ca(WO4) |
| Ca | Calcium | |
| Ca | ⓘ Scheelite | Ca(WO4) |
| W | Tungsten | |
| W | ⓘ Scheelite | Ca(WO4) |
| Au | Gold | |
| Au | ⓘ Native Gold | Au |
Other Databases
| Link to USGS - Alaska: | ID025 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Angayucham TerraneAccretionary Complex
- Farewell buried DomainDomain
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.