|Current site name||Unnamed (south of the Hammond River)|
|Geographic coordinates:||-149.98335, 67.6297 (WGS84)|
|Relative position||This site is at an elevation of about 4,300 feet, on a ridge south of the Hammond River, approximately 6 1/2 miles west-northwest of Sukakpak Mountain and 5 1/2 miles north of Jennie Creek Lake (SW1/4 sec. 3, T. 32 N., R. 11 W., of the Fairbanks Meridian). This site corresponds to unnamed loc. 76 in DeYoung (1978). The location is accurate within a 1-mile radius.|
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|Host or associated||Associated|
|Rock type||Sedimentary Rock > Carbonate > Limestone|
|Rock unit name||Skajit Limestone|
|Rock description||Skajit Limestone|
|Host or associated||Host|
|Rock type||Sedimentary Rock > Clastic Sedimentary Rock > Siltstone|
|Agency||Database name||Acronym||Record ID||Notes|
|USGS||Mineral Resources Data System||MRDS||A012154|
|USGS||Alaska Resource Data File||ARDF||CH082|
Brosgi, W.P., and Reiser, H.N., 1964, Geologic map and section of the Chandalar quadrangle, Alaska: U.S. Geological Survey Miscellaneous Geologic Investigations Map 1-375, 1 sheet, scale 1:250,000.
Cobb, E.H., 1972, Metallic mineral resources map of the Chandalar quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-457, 1 sheet, scale 1:250,000.
Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Chandalar and Wiseman quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-340, 205 p.
Grybeck, D.J., 1977, Known mineral deposits of the Brooks Range, Alaska: US Geological Survey Open-File Report 77-166C, 41 p., 1 sheet, scale 1:1,000,000.
DeYoung, J.H., Jr., 1978, Mineral resources map of the Chandalar quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-878-B, 2 sheets, scale 1:250,000.
Cobb, E.H., and Cruz, E.L., 1983, Summaries of data and lists of references to metallic and selected nonmetallic mineral deposits in the Chandalar quadrangle, Alaska: U.S. Geological Survey Open-File Report 83-278, 91 p.
|Subject category||Comment text|
|Deposit||Other Comments = A small outcrop, mapped by Dillon and Reifenstuhl (1995) as andesite tuff-dacite flow, is located adjacent to the conglomerate unit about 1/2 mile southeast of the Cu occurrence. This occurrence is located within Gates of the Arctic National Park.|
|Reporter||17-NOV-1999||J.M. Britton||U.S. Geological Survey|