Mogul

Prospect, Probably inactive

Commodities and mineralogy

Main commodities Fe
Ore minerals limonite

Geographic location

Quadrangle map, 1:250,000-scale NM
Quadrangle map, 1:63,360-scale D-2
Latitude 64.7619
Longitude -165.7313
Nearby scientific data Find additional scientific data near this location
Location and accuracy The Mogul prospect is on a rolling hill south of the divide between Trinity Creek to the west and Durrant Creek to the east. It is about 1.5 miles northeast of the Monarch prospect (NM017) and 1.5 miles south-southeast of the Tub Mountain prospect (NM018). The location is the approximate center of a group of limonite occurrences mapped by Herreid (1970). The location is accurate. This is locality 4 of Cobb (1972 [MF 463], 1978 [OFR 78-93]).

Geologic setting

Geologic description

The Mogul prospect includes four small concentrations of limonite at or near a contact of marble and schist (Herreid, 1970, figure 1). This prospect is one of several carbonate-hosted, iron-rich deposits in the area (NM014, NM014, NM017, NM018, and NM019). The limonite can be massive to granular, botryoidal, mammillary, or fibrous and commonly occurs in veins along joints and fractures in marble. The iron content ranges to as much as 59 percent in analyzed samples (Eakin, 1915 [B 622-I, p. 361-365]). Hematite, pyrolusite, and calcite are present locally. Shallit (1942; Mulligan and Hess, 1965, table 3) estimated that the Mogul prospect contains 5,000 long tons of rock with 10 to 20 percent iron.
This prospect and other iron deposits of the Sinuk River area occur at or near the base of massive marble whose protolith age is probably lower Paleozoic (Sainsbury, Hummel, and Hudson, 1972; Bundtzen and others, 1994). The deposits are locally controlled by high-angle faults or folds, but they are in general crudely stratabound within the basal massive marble or underlying calc-schist (Mulligan and Hess, 1965; Herreid, 1970). This stratigraphic interval also hosts base metal sulfide-fluorite-barite deposits at the Galena (NM130) and Quarry prospects (NM135).
The origin and age of the iron deposits of the Sinuk River area are uncertain. The deposits may be, in part, gossan developed on oxidized sulfide deposits (Eakin, 1915 [B 622-I, p. 361-365]; Mertie, 1918 [B 662-I, p. 425-449]; Cathcart, 1922; Mulligan and Hess, 1965; Herreid, 1970). Several of the iron deposits, including American (NM014) and Monarch (NM017), are locally highly anomalous in zinc and lead. Arguing against a simple gossan origin is the paucity of diagnostic textures and structures in boxworks that would suggest derivation from specific sulfide minerals. Alternatively, these deposits could be hypogene iron oxide and carbonate deposits probably transitional to lead-zinc-barite deposits such as the Quarry (NM135).
The age of the iron deposits of the Sinuk River area is most likely post-mid-Cretaceous because faults that crosscut mid-Cretaceous metamorphic rocks are an important control on them. A Late Cretaceous age for the iron deposits was suggested by Brobst and others (1971) as this is the age of flourine-rich tin granites of northwestern Seward Peninsula (Hudson and Arth, 1983). The youngest possible age appears to be Early Tertiary, when deep weathering, sandstone-type uranium mineralization, and possibly karst formation occurred to the east in the Solomon quadrangle (Hudson, 1999).
Geologic map unit (-165.733936475437, 64.7611362067716)
Mineral deposit model Carbonate-hosted, iron oxide deposit.
Age of mineralization Late Cretaceous or Early Tertiary; post mid-Cretaceous metamorphism.
Alteration of deposit Dolomitization and oxidation.

Production and reserves

Workings or exploration There may be small prospecting pits at this locality.
Indication of production None
Reserve estimates Shallit (1942); Mulligan and Hess, 1965, table 3) estimated that the Mogul prospect contains 5,000 long tons of rock with 10 to 20 percent iron.

References

MRDS Number A012780

References

Hudson, T.L., and Arth, J. G., 1983, Tin granites of Seward Peninsula, Alaska: Geological Society of America Bulletin, v. 94, p. 768-790.
Reporters C.C. Hawley and Travis L. Hudson
Last report date 10/22/1999