| Lat / long: | 64.99968, -147.74896 |
| Primary: | Gold |
| Ore: | Gold |
| Operation type: | Unknown |
| Development status: | Prospect |
| Alteration processes: | The intrusive at the surface is moderately to strongly silicified, locally bleached, and iron stained. The schist country rock is strongly silicified at the intrusive contact. Downhole, the sill is cut by sparse hairline quartz veinlets. In the shear zone, intrusive fragments are highly silicified and locally altered to clay (Dashevsky, 1993). |
| DEP | 10307445 |
| Reference | {Deposit:: Robinson, M.S., and Bundtzen, T. K., 1982, Geology of the Scrafford antimony-gold lode deposit, Fairbanks mining district, Alaska: Alaska Division of Geological and Geophysical Surveys Open-File Report 173, 7 p., 1 sheet, scale 1:120.}{Deposit:: Dashevsky, S.S., 1993, Eagle Creek project (Au), Fairbanks district, Alaska: American Copper and Nickel Company, Inc., 60 p. (Report held by Sam Dashevsky, Northern Associates Inc., Fairbanks, Alaska; can be examined with permission from current lease holders).} |
| Reporter | J.R. Guidetti Schaefer and C.J. Freeman |