|Quadrangle map, 1:250,000-scale||MC|
|Quadrangle map, 1:63,360-scale||A-3|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is on the east bank of lower Goat Creek. It is at an elevation of about 1,700 feet, about 1,000 feet south-southeast of elevation 2420 in the NE1/4 of section 30, T. 9 S., R. 19 E. of the Copper River Meridian. This is locality 17 of MacKevett (1976); the location is accurate to within about 1,000 feet.|
Geologic descriptionThis occurrence consists of a one-meter-wide altered quartz vein that is localized in a shear zone that cuts Permian marble and amphibolite. A grab sample of the quartz vein contained 1 part per million (ppm) silver, 500 ppm copper, and 50 ppm molybdenum (MacKevett, 1976).
|Geologic map unit||(-142.104008418196, 61.0620729234383)|
|Age of mineralization||Permian or younger based on the age of the marble and amphibolite the veins cut.|
|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|