Upper South Currant Creek Occurrence, Bristol Bay Mining District, Lake and Peninsula Borough, Alaska, USAi
Regional Level Types | |
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Upper South Currant Creek Occurrence | Occurrence |
Bristol Bay Mining District | Mining District |
Lake and Peninsula Borough | Borough |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
60° 16' 26'' North , 153° 32' 56'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
202740
Long-form identifier:
mindat:1:2:202740:4
GUID (UUID V4):
cc2b2b38-5204-42aa-925c-3036fea5dbab
Site is in Lake Clark National Park and Preserve.
Location: Located about 800 m north of the headwaters of South Currant Creek. Locality 28 of Nelson and others (1985) and locality 30 of MacKevett and Holloway (1977). SW1/4 sec. 12, T. 2 N., R. 25 W., of the Seward Meridian. Locality is accurate to within 750 m.
Geology: No detailed description of the mineralization was found in the literature. Weak mineralization (Resource Associates of Alaska, 1976) associated with the contact between Cretaceous granodiorite and Tertiary granites (Nelson and others, 1983; units Ki9 and Ti12). Unit Ki9 as a medium-grained granodiorite with compositional ranges from silicic granodiorite to mafic tonalite and quartz diorite. Rocks near the margin of the pluton contain lesser quartz and fall within the quartz diorite field. Unit Ti12 is described as coarse-grained biotite granite (North of Currant Creek) and medium- to coarse-grained granodiorite (South of Currant Creek).
Workings: Unknown
Age: Tertiary or younger.
Alteration: Unknown
Production: No production
Reserves: No reserves
Commodities (Major) - Cu; (Minor) - Mo
Development Status: None
Deposit Model: Porphyry Cu ? (Cox and Singer, 1986; model 17 ?)
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: | LC039 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
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