Main commodities | Cu |
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Ore minerals | chalcopyrite; pyrite |
Quadrangle map, 1:250,000-scale | MC |
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Quadrangle map, 1:63,360-scale | D-1 |
Latitude | 61.9825 |
Longitude | -141.0879 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This prospect is on the south side of a small, unnamed east tributary to Beaver Creek. It is at an elevation of about 3,700 feet about 2,000 feet west of the center of section 6, T. 2 N., and R. 24 E. of the Copper River Meridian. This is locality 188 of MacKevett (1976). |
Geologic descriptionThe deposit at this prospect consists of pyrite and minor chalcopyrite in veins and as disseminations in granodiorite and in adjacent hornfels roof pendants (Moffit and Knopf, 1910; MacKevett, 1976). The prospect is on the south side of a prominent shear zone that trends east-west along an unnamed tributary to Beaver Creek (Knaebel, 1970). Bedrock in the area is Jurassic or Cretaceous siliciclastic rocks intruded by Cretaceous granitic rocks (MacKevett, 1978). | |
Geologic map unit | (-141.090021340207, 61.9821718228074) |
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Age of mineralization | Cretaceous? The mineralization appears to be related to the emplacement of Cretaceous granitic rocks. |
Alteration of deposit | Oxidation. Rusty exposures mark the mineralization (Knaebel, 1970). |
Workings or exploration | Probably some minor workings. |
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Indication of production | None |
Additional commentsThe locality is in the Wrangell-Saint Elias National Park and Preserve. |
MRDS Number | A011770 |
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References | |
Reporters | Travis L. Hudson (Applied Geology, Inc.) |
Last report date | 1/12/2003 |