|Quadrangle map, 1:250,000-scale||HE|
|Quadrangle map, 1:63,360-scale||D-3|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is at an elevation of about 3,700 feet on the north wall of the valley of Cody Creek, about 3.8 miles upstream from its junction with Wood River. The map site is in the NE1/4 of sec. 34, T. 12 S., R. 3 W., of the Fairbanks Meridian. The location is accurate to within 0.5 mile.|
Geologic descriptionThe country rocks in the area of this occurrence are Lower Paleozoic or possibly Upper Precambrian schists, cut by Upper Cretaceous stocks and Tertiary sills and dikes. Limited information about this deposit suggests that it consists of one or more stibnite-quartz veins. Such a deposit would be of interest chiefly for its gold context.
|Geologic map unit||(-148.112317415332, 63.8395568482562)|
|Mineral deposit model||Simple Sb (Cox and Singer, 1986; model 27d)|
|Mineral deposit model number||27d|
|Age of mineralization||Probably Late Cretaceous or younger.|
|Workings or exploration||There has been surface exploration only.|
|Indication of production||None|
Cobb, E.H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Healy quadrangle, Alaska: U.S. Geological Survey Open-File Report 78-1062, 113 p.
|Reporters||N. Van Wyck (Stevens Exploration Management Corporation)|
|Last report date||4/7/2000|