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Hungry Creek Mine, Nome Mining District, Nome Census Area, Alaska, USAi
Regional Level Types
Hungry Creek MineMine
Nome Mining DistrictMining District
Nome Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 39' 59'' North , 165° 41' 49'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Nome3,806 (2018)23.0km
Mindat Locality ID:
198082
Long-form identifier:
mindat:1:2:198082:3
GUID (UUID V4):
0


Location: Hungry Creek is an east tributary of Oregon Creek. The mouth of Hungry Creek is three quarters of a mile upstream of the junction of Oregon Creek and Cripple River at the Nome-Teller road. It has been mined for about 2 miles from near its mouth upstream nearly to an auriferous south branch called May Creek (NM176). The coordinate location is the approximate mid-point of the workings; it is accurate to within about 1,000 feet. This is locality 76 of Cobb (1972 [MF 463], 1978 [OFR 78-93]).
Geology: Placer gold mining on Hungry Creek began soon after discovery in July, 1900. In 1903, there were three mines in operation, but most of the creek had some prospecting or mining by then (Collier and others, 1908). The creek had numerous rounded granitic boulders, derived from the Kigluaik Mountains; some of the pay gravel was decomposed chloritic schist fragments with intermixed boulders. Gold was accompanied by a small quantity of rounded bismuth nuggets as much as an ounce in weight. Magnetite was the most abundant mineral in the associated heavy mineral concentrates. In addition to mining on one of its headwater tributaries, May Creek (NM176), a small north tributary called Trilby Creek (NM177) was also placer mined. Trilby Creek is possibly located along the Aurora fault of Bundtzen and others (1994). The lower part of Hungry Creek locally flows over dolostone. The dolostone may be alteration products like the dolostone at the many iron oxide deposits of the Sinuk River area (Bundtzen and others, 1994); an example is the nearby Cleveland occurrence (NM161). Bedrock on a part of the creek above a strong northeast fault is mainly the porphyroclastic graphitic schist unit of Bundtzen and others (1994). The fault, named the Aurora fault by Bundtzen and others (1994), is locally mineralized with antimony or gold (see NM157, for example).
Workings: Small-scale surface workings are present.
Age: Quaternary.

Commodities (Major) - Au; (Minor) - Bi, Fe, Ti
Development Status: Yes; small
Deposit Model: Alluvial placer Au (Cox and Singer, 1986; model 39a).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Gold1.AA.05Au
ⓘNative Bismuth1.CA.05Bi
Group 4 - Oxides and Hydroxides
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘIlmenite4.CB.05Fe2+TiO3
ⓘRutile4.DB.05TiO2
Unclassified
ⓘ'Garnet Group'-X3Z2(SiO4)3

List of minerals for each chemical element

OOxygen
Oⓘ IlmeniteFe2+TiO3
Oⓘ MagnetiteFe2+Fe23+O4
Oⓘ RutileTiO2
Oⓘ Garnet GroupX3Z2(SiO4)3
SiSilicon
Siⓘ Garnet GroupX3Z2(SiO4)3
TiTitanium
Tiⓘ IlmeniteFe2+TiO3
Tiⓘ RutileTiO2
FeIron
Feⓘ IlmeniteFe2+TiO3
Feⓘ MagnetiteFe2+Fe23+O4
AuGold
Auⓘ Native GoldAu
BiBismuth
Biⓘ Native BismuthBi

Other Databases

Link to USGS - Alaska:NM149

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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