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Starship Prospect, Yukon-Koyukuk Census Area, Alaska, USAi
| Regional Level Types | |
|---|---|
| Starship Prospect | Prospect |
| Yukon-Koyukuk Census Area | Census Area |
| Alaska | State |
| USA | Country |
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Latitude & Longitude (WGS84):
63° 28' 58'' North , 154° 4' 33'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
See Spring Ridge (MD047), Bear Pass (MD044), Beaver (MD048), and Big Gate (MD050) Mississippi Valley Type occurrences in Medfra quadrangle. The Starship prospect is on land selected or conveyed to Doyon Ltd. For further information, contact Doyon Ltd. at 210 1st Ave., Fairbanks, Alaska, 99701.
Location: The Starship prospect is located about one mile (1.5 km) northeast of the Bear Pass prospect on a northwest facing ridgeline at an elevation of 2,150 feet (655 m) in Section 20, T. 23 S., R. 25 E., of the Kateel River Meridian. Location is known to within about 125 feet (38 m).
Geology: The Starship prospect consists of a smithsonite-bearing solution breccia in dolomite and limestone of the Paradise Fork Formation of Dutro and Patton (1982); this is unit 'Sic' of Andrews and Rishel (1982). Zone of mineralization measures about 15 feet by 100 feet (4.5 m by 30 m) and is mainly in rubble crop. Age of host unit is Silurian (inferred), based on fossil control. (Patton and others, 1980; Dutro and Patton, 1982; Schmidt, 1997). The age of the mineralization is unknown. Grab samples from surface explorations of high grade mineralization contain up to 23.25 percent zinc and 0.14 percent cadmium. Mineralized rubble crop distribution indicates a relatively small and discordant mineral body.
Workings: The Starship prospect was found by WGM Inc. and Patino Ltd. in the late 1970s during base metal exploration on lands selected by Doyon Ltd (Andrews and Rishel, 1982). Grab samples from surface explorations of high grade mineralization contain up to 23.25 percent zinc and 0.14 percent cadmium. Mineralized rubble crop distribution indicates a relatively small and discordant mineral body.
Age: Age of host unit is Silurian (inferred), based on fossil control. (Dutro and Patton, 1982). The age of mineralization is unknown.
Alteration: Secondary dolomite.
Reserves: None.
Commodities (Major) - Zn; (Minor) - Cd
Development Status: No
Deposit Model: Southeast Missouri Pb-Zn (Cox and Singer, 1986; model no. 32a) or Mississippi V
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.
Detailed Mineral List:
| ⓘ Smithsonite Formula: ZnCO3 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 5 - Nitrates and Carbonates | |||
|---|---|---|---|
| ⓘ | Smithsonite | 5.AB.05 | ZnCO3 |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Smithsonite | ZnCO3 |
| O | Oxygen | |
| O | ⓘ Smithsonite | ZnCO3 |
| Zn | Zinc | |
| Zn | ⓘ Smithsonite | ZnCO3 |
Other Databases
| Link to USGS - Alaska: | MD043 |
|---|
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
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