|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 2.2 miles south of the east end of Ernie Lake. The occurrence is at the top of a ridge at an elevation of about 1,320 meters, about 0.4 mile west of the top of hill 1425, in the NW1/4 section 8, T. 29 N., R. 25 W of the Fairbanks Meridian. This occurrence is the site of sample 54 in Dillon and others (1981 [AOF 133B]). The location is accurate.|
Geologic descriptionThis occurrence consists of chlorite-talc-quartz schist with lenses of pyrite and galena(?) less than 6 cm long (Dillon and others, 1981 [AOF 133B]). The rocks in the area consist of Devonian, Skajit Limestone and/or Proterozoic(?) banded schist (Dillon and others, 1986).
|Geologic map unit||(-152.971364623671, 67.3560276679314)|
|Workings or exploration||Only surface sampling.|
|Indication of production||None|
Additional commentsThis occurrence is in Gates of the Arctic National Park.
|Reporters||J.M. Britton (Anchorage)|
|Last report date||8/9/2002|