|Quadrangle map, 1:250,000-scale||NT|
|Quadrangle map, 1:63,360-scale||C-3|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||The occurrence is located near the head of Rabbit Creek at an elevation of about 825 feet; it is about 0.3 mile northeast of the center of Section 10, T. 26 N., R. 21 W., of the Kateel River Meridian. The location is accurate.|
Geologic descriptionStratiform(?) base metal mineralization occurs in light-gray- and tan-weathering phyllite of the Devonian to Permian(?) Endicott Group. The occurrence was found by a mineral exploration firm working for NANA Regional Corporation, Inc., and briefly noted by the U.S. Bureau of Mines (1980). One sample with 3 percent pyrite contained 2.5 percent lead, 0.85 percent zinc, and 4.5 ounces of silver per ton.
|Geologic map unit||(-163.380493013296, 67.6685297981451)|
|Mineral deposit model||Stratiform Ag-Pb-Zn deposit.|
|Age of mineralization||Devonian to Permian based on the age of the host rock.|
|Workings or exploration||Limited sampling by a exploration company.|
|Indication of production||None|
Additional commentsThis occurrence is now within the Cape Krusenstern National Monument which is closed to mining and mineral exploration.
U.S. Bureau of Mines, 1980, Mineral deposits of the Cape Krusenstern area, Alaska: A preliminary report: U.S. Bureau of Mines Open File Report 42-80, 22 p.
|Reporters||J. M. Schmidt and J.A. Dumoulin (U.S. Geological Survey)|
|Last report date||10/14/1996|