|Quadrangle map, 1:250,000-scale||MC|
|Quadrangle map, 1:63,360-scale||C-8|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is on the ridge north of upper Slatka Creek. It is at an elevation of about 6,200 feet, 2,400 feet south of the center of section 17, T. 3 S., R. 10 E. of the Copper River Meridian. This is locality 125 of MacKevett (1976); the location is accurate to within about 1,000 feet.|
Geologic descriptionThis occurrence consists of patchy altered zones that are locally present in Triassic Nikolai Greenstone (MacKevett, 1976). A sample of the altered material contained 700 parts per million (ppm) copper and 500 ppm zinc.
|Geologic map unit||(-143.654386049733, 61.5988445856305)|
|Mineral deposit model||Disseminated sulfides|
|Age of mineralization||Triassic or younger based on the age of the host rocks.|
|Alteration of deposit||The type of alteration was not specified.|
|Workings or exploration||Only limited surface sampling.|
|Indication of production||None|
Additional commentsThe locality is in the Wrangell-Saint Elias National Park and Preserve.
|Reporters||Travis L. Hudson (Applied Geology, Inc.)|
|Last report date||1/12/2003|