|Quadrangle map, 1:250,000-scale||CR|
|Quadrangle map, 1:63,360-scale||A-1|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||These prospects are scattered for about a mile along an east-west trend; their midpoint is about 0.4 mile south-southwest of hill 2221 and about 0.5 mile west-southwest of the center of section 35, T. 77 S., R. 88 E., of the Copper River Meridian.|
Geologic descriptionThe only evidence for these prospects is that they are shown on an old, small-scale map by Wright and Wright (1908, figure 18). Hedderly-Smith (1999 [Inventory]) refers to them in passing in describing geochemical anomalies in the area. The rocks in the area are schist and marble of the Wales Group of Late Proterozoic and Cambrian age (Eberlein and others, 1983; Brew, 1996).
|Geologic map unit||(-132.122961981627, 55.1463645594677)|
|Indication of production||None|
Brew, D.A., 1996, Geologic map of the Craig, Dixon Entrance, and parts of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-2319, 53 p., 1 sheet, scale 1:250,000.
Eberlein, G.D., Churkin, Michael, Jr., Carter, Claire, Berg, H.C., and Ovenshine, A. T., 1983, Geology of the Craig quadrangle, Alaska: U.S. Geological Survey Open-File Report 83-91, 52 p.
Hedderly-Smith, D.A., 1999, Inventory of metallic mineral prospects, showings and anomalies on Sealaska lands, 1988 through 1998: Sealaska Corporation, Juneau, Alaska, 217 p. (internal report held by Sealaska Corporation, Juneau, Alaska).
|Reporters||D.J. Grybeck (Applied Geology)|
|Last report date||5/1/2004|