|Quadrangle map, 1:250,000-scale||LG|
|Quadrangle map, 1:63,360-scale||C-3|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||SE1/4SE1/4 sec. 21, T. 8 N., R. 4 W., of the Fairbanks Meridian. This occurrence is approximately 1.5 miles east of Amy Dome.|
Geologic descriptionCinnabar occurs in disseminations and quartz veins in altered granite dikes and plutons that intrude Ordovician to Devonian siltstone and argillite (Robinson and others, 1982).
|Geologic map unit||(-148.369504292393, 65.4995681242996)|
|Mineral deposit model||Cinnabar-quartz vein.|
|Age of mineralization||Host rock is Late Cretaceous to early Tertiary granite.|
|Indication of production||None|
Additional commentsThis site was referred to as the 'Hudson Cinnabar' prospect in Nokleberg and others (1987), but it is in a different location than the Hudson cinnabar mine on Olive Creek (ARDF no. LG015).
Nokleberg, W.J., Bundtzen, T.K., Berg, H.C., Brew, D.A., Grybeck, D.J., Robinson, M.S., Smith, T.E., and Yeend, W., 1987, Significant metalliferous lode deposits and placer districts of Alaska: U.S. Geological Survey Bulletin 1786, 104 p., 2 plates, scale 1:5,000,000.
|Reporters||C.J. Freeman, J.R. Guidetti Schaefer (Avalon Development Corporation)|
|Last report date||5/4/1999|