|Quadrangle map, 1:250,000-scale||MC|
|Quadrangle map, 1:63,360-scale||B-3|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is on the west valley wall of upper Hawkins Glacier. It is at an elevation of about 5,500 feet, 5,000 feet southeast of peak 11040 in the NE1/4 of section 30, T. 6 S., R. 20 E. of the Copper River Meridian. This is locality 43 of MacKevett (1976); the location is probably accurate to within 500 feet.|
Geologic descriptionThis occurrence is in altered Tertiary granodiorite. A sample contained 7 parts per million (ppm) silver, 200 ppm bismuth, and 500 ppm molybdenum (MacKevett, 1976).
|Geologic map unit||(-141.891132266519, 61.3189936973933)|
|Mineral deposit model||Porphyry Mo, low F? (Cox and Singer, 1986; model 21b)|
|Mineral deposit model number||21b?|
|Age of mineralization||Tertiary based on the age of the granodiorite host rock.|
|Workings or exploration||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|