Boulder Creek Occurrence, Yukon-Koyukuk Census Area, Alaska, USAi
| Regional Level Types | |
|---|---|
| Boulder Creek Occurrence | Occurrence |
| 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):
63° 18' 36'' North , 154° 37' 47'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Location: The Boulder Creek placer occurrence is located in Boulder Creek valley at an elevation of 1,000 feet (304 m) in Section 11, T. 25 S., R. 22 E., of the Kateel River Meridian. Location is imprecisely known and judged to be within a two mile (3.2 km) radius.
Geology: Placer gold was found in the valley of Boulder Creek, a third order tributary of the Nixon Fork, in 1920 (Brown, 1926). No bedrock is exposed and no gravel thicknesses are known. Age of mineralization is unknown.
Reserves: None.
Commodities (Major) - Au; (Minor) - Ag
Development Status: No
Deposit Model: Placer Au-PGE (Cox and Singer, 1986; model no. 39c)
Commodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.List of minerals for each chemical element
Other Databases
| Link to USGS - Alaska: | MD057 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Farewell-McGrath DomainDomain
- Farewell TerranePassive Margin
USA
- Alaska
- Yukon-Koyukuk Census Area
- McGrath Mining DistrictMining District
- Yukon-Koyukuk Census Area
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.