|Quadrangle map, 1:250,000-scale||MC|
|Quadrangle map, 1:63,360-scale||A-4|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is on a small bedrock knob on the south bank of the Chitina River flood plain. It is at an elevation of about 1,600 feet, about 0.9 mile northeast of the mouth of McCurdy Creek near the center of the south 1/2 of section 14, T. 9 S., R. 18 E. of the Copper River Meridian. This is locality 18 of MacKevett (1976); the location is accurate to within about 1,000 feet.|
Geologic descriptionThis occurrence consists of a quartz vein in a fault in Permian marble. A sample contained 1 part per million silver and 70 parts per million molybdenum (MacKevett, 1976).
|Geologic map unit||(-142.167212379178, 61.0842724692423)|
|Mineral deposit model||Quartz vein|
|Age of mineralization||Permian or younger based on the age of the marble host rock.|
|Alteration of deposit||Silicification.|
|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|