|Quadrangle map, 1:250,000-scale||EA|
|Quadrangle map, 1:63,360-scale||B-1|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||Smith Creek is a 12-mile-long south tributary of the lower Fortymile River, located about 3 miles west of the Canadian border and about 2 miles south of the Eldon landing strip. Pay was found for at least 2 miles along Smith Creek. The coordinates are placed about 1 mile upstream of the mouth of the creek, in section 6, T. 8 S., R. 34 E., of the Fairbanks Meridian. The location is accurate within 1 mile. Smith Creek is locality 54 of Eberlein and others (1977).|
The rocks along most of Smith Creek are Paleozoic gneiss, schist, amphibolite, quartzite, and marble (Foster, 1969 [B 1271-G]). Dioritic to granodioritic gneiss and graphitic quartzite and quartz-muscovite schist of the Nasina Series of Devonian to Mississippian age crop out at the head of Smith Creek (Mortensen, 1988; Mortensen, 1999). Extensive terrace gravel deposits occur on both sides of the lower portion of the Fortymile River (see EA071), including in the Smith Creek valley.Gold-bearing gravels were found for at least 2 miles along Smith Creek and its benches, but the creek was not regarded as rich (Powers, 1935). Mining occurred on Smith Creek in 1932 (Smith, 1934 [B 857-A]), and two men were working on Smith Creek in the mid-1930s (Powers, 1935). There was prospecting on Smith Creek in 2000 (R.L. Flynn, unpub. data, 2000). Placer gold has also been produced on the lower Fortymile River near the mouth of Smith Creek.
|Geologic map unit||(-141.081466425986, 64.2534922167811)|
|Mineral deposit model||Placer Au (Cox and Singer, 1986; model 39a).|
|Mineral deposit model number||39a|
|Age of mineralization||Quaternary.|
|Workings or exploration||Gold-bearing gravels were found for at least 2 miles along Smith Creek and its benches, but the creek was not regarded as rich (Powers, 1935). Mining occurred on Smith Creek in 1932 (Smith, 1934 [B 857-A]), and two men were working on Smith Creek in the mid-1930s (Powers, 1935). There was prospecting on Smith Creek in 2000 (R.L. Flynn, unpub. data, 2000). Placer gold has also been produced on the lower Fortymile River (see EA071) near the mouth of Smith Creek.|
|Indication of production||Yes; small|
Cobb, E.H., 1977, Summary of references to mineral occurrences in the Eagle quadrangle, Alaska: U.S. Geological Survey Open-File Report 77-845, 122 p.
Eberlein, G.D., Chapman, R.M., Foster, H.L., and Gassaway, J.S., 1977, Map and table describing known metalliferous and selected nonmetalliferous mineral deposits in central Alaska: U.S. Geological Survey Open-File Report 77-168-D, 132 p., 1 sheet, scale 1:1,000,000.
Foster, H.L., 1969, Reconnaissance geology of the Eagle A-1 and A-2 quadrangles, Alaska: U.S. Geological Survey Bulletin 1271-G, p. G1-G30.
Foster, H.L., and Keith, T.C., 1968, Preliminary geologic map of the Eagle B-1 and C-1 quadrangles: U.S. Geological Survey Open-File Report 68-103, 1 sheet, scale 1:63,360.
Mortensen, J. K., compiler, 1988, Geology, southwestern Dawson map area, Yukon Territory (NTS 116B, C): Geological Survey of Canada Open File 1927, 1 sheet, scale 1:250 000.
Mortensen, J.K. (compiler), 1999, Yukonage--An isotopic age database for the Yukon Territory, in Gordey, S.P., and Makepeace, A.J., compilers, Yukon Digital Geology: Indian and Northern Affairs Canada, Exploration and Geological Services Division, Yukon Region.
Powers, J.B., 1935, Synopsis and history of early day mining and prospecting on the Fortymile River and its bars and low benches: Alaska Territorial Department of Mines Miscellaneous Report 60-2, 19 p.
|Reporters||R.L. Flynn; M.B. Werdon|
|Last report date||5/1/2002|