Quadrangle map, 1:250,000-scale | MC |
---|---|
Quadrangle map, 1:63,360-scale | B-4 |
Latitude | 61.3122 |
Longitude | -142.1646 |
Nearby scientific data | Find additional scientific data near this location |
Location and accuracy | This occurrence is on the west valley wall of an unnamed north tributary to Canyon Creek. It is at an elevation of about 5,200 feet, about 2,600 feet north-northwest of the center of section 34, T. 6 S., R. 18 E. of the Copper River Meridian. This is locality 45 of MacKevett (1976); the location is accurate to within about 1,000 feet. |
Geologic descriptionThis occurrence consists of irregular altered zones in upper Paleozoic volcaniclastic rocks (MacKevett and Smith, 1968; MacKevett, 1976). A sample of the altered rock contained 5.2 parts per million gold. | |
Geologic map unit | (-142.166637229366, 61.3117829496882) |
---|---|
Age of mineralization | Upper Paleozoic or younger based on the age of the host rocks. |
Workings or exploration | Limited surface sampling. |
---|---|
Indication of production | None |
Additional commentsThe locality is in the Wrangell-Saint Elias National Park and Preserve. |
References | |
Reporters | Travis L. Hudson (Applied Geology, Inc.) |
---|---|
Last report date | 1/12/2003 |