Slate Creek

Occurrence, Inactive

Commodities and mineralogy

Main commodities Cu; Mn
Ore minerals chalcopyrite; rhodonite

Geographic location

Quadrangle map, 1:250,000-scale CH
Quadrangle map, 1:63,360-scale A-6
Latitude 67.18
Longitude -149.86
Nearby scientific data Find additional scientific data near this location
Location and accuracy The Slate Creek lode occurrence is located at an elevation of about 3,100 ft approximately 4 miles southeast of the Myrtle Creek landing strip (sec. 12, T. 27 N., R. 11 W., of the Fairbanks Meridian). The location is accurate within a 1/2-mile radius.

Geologic setting

Geologic description

The occurrence is described as blocks of talus as much as 30 cm in diameter of pink- and cream-colored silicates with manganese values as much as 22.23 percent (Fechner and others, 1993). Manganese oxide-stained chert with fine- to coarse-grained chalcopyrite was found nearby. The mineralized chert gave values of as much as 16.36 percent Mn. The manganese-mineralized rubble crops do not extend more than 30 m in any direction. The area is mapped by Brosgé and Reiser (1964) as within the chert unit of a Devonian(?) sequence of volcanic rocks and chert.
Geologic map unit (-149.862716781187, 67.1795726530798)
Mineral deposit model Volcanogenic Mn? (Cox and Singer, 1986; model 24c?).
Mineral deposit model number 24c?

Production and reserves

Workings or exploration No known activity.
Indication of production None

References