Main commodities | Cu; Mo |
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Ore minerals | chalcopyrite; molybdenite |
Quadrangle map, 1:250,000-scale | VA |
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Quadrangle map, 1:63,360-scale | B-1 |
Latitude | 61.495 |
Longitude | -144.259 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is located on a low ridge along the west side of the Chitina River, about 500 feet south of the north boundary of the Valdez B-1 topographic map. It is in the NE1/4 section 26, T. 4 S., R. 6 E., of the Copper River Meridian. This prospect is probably located to within one-quarter mile; it is locality 61 of Winkler and others (1981 [OFR 80-892-B]). |
Geologic descriptionSparse chalcopyrite and molybdenite are disseminated in Jurassic (?) biotite granodiorite (Winkler and others, 1981 [OFR 80-892-B]; Winkler and others, 1981 [OFR 80-892-A]). The pluton is in metamorphic rocks that include mafic metavolcanic rocks of the Paleozoic Skolai Group. | |
Geologic map unit | (-144.261087802176, 61.4945284669807) |
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Mineral deposit model | Porphyry Cu-Mo (Cox and Singer, 1986; model 21a) |
Mineral deposit model number | 21a |
Age of mineralization | Jurassic?; the probable age of the granodiorite host rock (Winkler and others, 1981 [OFR 80-892-A]). |
Workings or exploration | Probably only reconnaissance surface examination. |
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Indication of production | None |
Additional commentsThis occurrence is in Wrangell-St. Elias National Park. |
MRDS Number | A011591 |
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References | |
Reporters | Travis L. Hudson |
Last report date | 12/14/2001 |