Unnamed Occurrence (ARDF - MM163; on a tributary to upper Pirate Creek), Kantishna Mining District, Denali Borough, Alaska, USAi
Regional Level Types | |
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Unnamed Occurrence (ARDF - MM163; on a tributary to upper Pirate Creek) | - not defined - |
Kantishna Mining District | Mining District |
Denali Borough | Borough |
Alaska | State |
USA | Country |
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Latitude & Longitude (WGS84):
63° 23' 6'' North , 150° 14' 34'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Mindat Locality ID:
201369
Long-form identifier:
mindat:1:2:201369:8
GUID (UUID V4):
faa3cefe-d3b2-4ffb-8733-3d56eb5f62d5
The occurrence is in Denali National Park and Preserve.
Location: This occurrence is on the west side of a north-flowing tributary of Pirate Creek about a mile west of Muldrow Glacier. It is probably within a few hundred feet of the north end of the section line between sections 29 and 30, T. 18 S., R. 15 W., Fairbanks Meridian. The occurrence is included in the description of the Twin Hills lode (MM168) by Cobb (1972, location 35 [MF 366]; 1980 [OFR 80-363]), and in the description of location 44 by MacKevett and Holloway (1977).
Geology: This occurrence is immediately east of the Twin Hills lode (MM168), in the contact zone of the McGonagall granitic pluton mapped by Reed (1961, plate 1). The deposit consists of replacement veins and disseminations of magnetite in a zone estimated to be 20 to 30 feet wide (Moffit, 1933, p. 324). A small amount of chalcopyrite occurs with the magnetite, and the rocks locally are ironstained and coated with copper carbonate(?). Sphalerite occurs in a fracture zone about 100 yards north of the magnetite deposit. The deposit probably is middle Tertiary, the approximate age of the emplacement of the Eocene or Oligocene McGonagall pluton (Reed and Lanphere, 1974). The occurence is one of several in a belt of mineral deposits along the north flank of the McGonagall pluton.
Workings: The deposit was discovered by W. J. Shannon in about 1930.
Age: The deposit probably is middle Tertiary, the approximate age of the emplacement of the Eocene or Oligocene McGonagall pluton (Reed and Lanphere, 1974; Cole, 1998).
Alteration: Oxidation of iron and copper minerals.
Commodities (Major) - Fe; (Minor) - Cu, Zn
Development Status: No
Deposit Model: Disseminated and vein-form, polymetallic lodes and contact deposits (Cox and Si
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
3 valid minerals.
Detailed Mineral List:
β Chalcopyrite Formula: CuFeS2 |
β 'Copper Stain' |
β 'Limonite' |
β Magnetite Formula: Fe2+Fe3+2O4 |
β Sphalerite Formula: ZnS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Sphalerite | 2.CB.05a | ZnS |
β | Chalcopyrite | 2.CB.10a | CuFeS2 |
Group 4 - Oxides and Hydroxides | |||
β | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
Unclassified | |||
β | 'Limonite' | - | |
β | 'Copper Stain' | - |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | β Magnetite | Fe2+Fe23+O4 |
S | Sulfur | |
S | β Chalcopyrite | CuFeS2 |
S | β Sphalerite | ZnS |
Fe | Iron | |
Fe | β Chalcopyrite | CuFeS2 |
Fe | β Magnetite | Fe2+Fe23+O4 |
Cu | Copper | |
Cu | β Chalcopyrite | CuFeS2 |
Zn | Zinc | |
Zn | β Sphalerite | ZnS |
Other Databases
Link to USGS - Alaska: | MM163 |
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Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Windy-McKinley DomainDomain
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