Main commodities | Cu |
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Ore minerals | chalcopyrite |
Quadrangle map, 1:250,000-scale | BN |
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Quadrangle map, 1:63,360-scale | B-2 |
Latitude | 65.48 |
Longitude | -162.54 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | French Creek is a south tributary to Holtz Creek, a west tribuary to Independence Creek. Sainsbury (1975, p. 85) originally described the location as a chalcopyrite vein in a limestone cliff on the north side of the headwaters to Independence Creek. The bedrock geology (Till and others, 1986) that best matches this location description is used here. This location is very approximate, probably within 1 to 2 miles. It is locality 33 of Gamble (1988). |
Geologic descriptionSainsbury (1975, p. 85) describes this occurrence as a 4 inch-wide chalcopyrite vein in a limestone (marble) cliff. This exposure is supposed to be on the north side of the headwaters to Independence Creek and near to a large magnetic anomaly. Till and others (1986) show exposures of Paleozoic marble on both sides of French Creek at this location. This is the only place in the headwaters of Independence Creek that the bedrock geology appears to match Sainsbury's (1975, p. 85) original description. | |
Geologic map unit | (-162.542658596563, 65.4793049564952) |
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Mineral deposit model | Sulfide vein in marble |
Age of mineralization | Cretaceous ?; Epigenetic mineralization in metamorphic rocks of Seward Peninsula is primarily of Cretaceous age. |
Workings or exploration | No workings are known at this location. |
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Indication of production | None |
MRDS Number | A012776 |
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References | |
Reporters | Travis L. Hudson (Applied Geology) |
Last report date | 3/15/1999 |