|Quadrangle map, 1:250,000-scale||WI|
|Quadrangle map, 1:63,360-scale||B-6|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is located about 4 miles northeast of Ernie Lake. The occurrence is at an elevation of about 1,700 meters, about 0.2 mile west-southwest of the center of section 14, T. 30 N., R. 24 W., of the Fairbanks Meridian. The occurrence is the site of sample 55 of Dillon and others (1981 [AOF 133B]). The location is accurate.|
Geologic descriptionThis occurrence consists of maroon, felsic schist that contains 5% oxidized sulfides (Dillon and others, 1981 [AOF 133B]). The sulfides are principally pyrite and sphalerite, and possibly galena. A rock sample contains 350 ppm Zn. The rocks in the area are Devonian, Skajit Limestone, a few miles south of the Earnie Lake pluton (Dillon and others, 1986). No other information is available.
|Geologic map unit||(-152.86126742302, 67.42343114106)|
|Mineral deposit model||Polymetallic replacement deposit? (Cox and Singer, 1986; model 19a?).|
|Mineral deposit model number||19a?|
|Alteration of deposit||Oxidation of sulfide minerals.|
|Workings or exploration||Only surface sampling.|
|Indication of production||None|
Additional commentsSee also: Buzz (WI047); Ann (WI034).
|Reporters||J.M. Britton (Anchorage)|
|Last report date||8/9/2002|