|Quadrangle map, 1:250,000-scale||SR|
|Quadrangle map, 1:63,360-scale||D-5|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||This occurrence is in the NE1/4 section 26, T. 9 N., R. 5 E., of the Seward Meridian. It is at an elevation of 800 feet on the east side of Seth Glacier valley about a mile north of the head of Poe Bay. This is location on S-167 of Jansons and others (1984). This location is accurate to within a quarter of a mile.|
Geologic descriptionThis occurrence is in sedimentary rocks of the Valdez Group of Late Cretaceous age (Jansons and others, 1984). It consists of a 3-inch-wide quartz vein containing considerable galena and pyrite. No other information or assay results are reported.
|Geologic map unit||(-148.50490496359, 60.8474096020766)|
|Mineral deposit model||Low-sulfide Au-quartz vein (Cox and Singer, 1986; model 36a)|
|Mineral deposit model number||36a|
|Age of mineralization||Cretaceous or younger; the vein cuts rocks of the Valdez Group of Late Cretaceous age.|
|Workings or exploration||This occurrence was discovered by Kurt Stuwe and reported to the U.S. Bureau of Mines in 1982 (Hoekzema and Sherman, 1983). No assay results have been reported.|
|Indication of production||None|
Hoekzema, R.P., and Sherman, G.E., 1983, Mineral investigations in the Chugach National Forest, Alaska (Peninsula study area): U.S. Bureau of Mines in-house report; held at U.S. Bureau of Land Management Alaska State Office, Anchorage, 524 p.
|Reporters||Jeff A. Huber (Anchorage)|
|Last report date||7/30/2000|