Unnamed Occurrence (ARDF - FP010), Alaska Peninsula District, Aleutians East Borough, Alaska, USA
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Location: Approximate location is about 5 km south of False Pass community. Anomaly no. 49 of Christie (1974) and no. 2 of MacKevett and Holloway (1977, p. 11). Location description is poor; however, location apparently is southwest of Whirl Point on Unimak Island.
Geology: Christie (1974) briefly examined a poorly defined color anomaly 2 mi (3.2 km) in diameter developed in andesitic volcanic flows, breccia, and tuff intruded by multiple diorite stocks(?). The diorite contact metamorphoses the volcanic rocks and pyrite is disseminated in both the diorite and the volcanic rocks. The diorite is pervasively propylitically altered.
Workings: Brief reconnaissance geologic mapping and a few silt samples were collected. One sample had 0.01 ppm gold. Occurrence apparently has not been adequately examined for epithermal gold vein potential.
Age: Miocene or younger
Alteration: Pervasive propylitic alteration of diorite within the color anomaly and local(?) silicification. Hydrothermal minerals reported include clay, chlorite, and epidote.
Commodities (Major) - Ag, Au?
Development Status: No
Deposit Model: Epithermal gold vein
Mineral List
1 entry listed. 1 valid mineral.
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References
Christie, J.S., 1974, Aleut-Quintana-Duval 1974 joint venture, final report: Unpublished Quintana Minerals Corporation report, 24 p., 3 appendices, 2 maps. (Report held by the Aleut Corporation, Anchorage, Alaska.) MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous mineral deposits in the western part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-F, 38 p., 1 sheet, scale 1:1,000,000.