Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Iron Creek Prospect, Nome Mining District, Nome Census Area, Alaska, USAi
Regional Level Types
Iron Creek ProspectProspect
Nome Mining DistrictMining District
Nome Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 44' 9'' North , 165° 44' 24'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Nome3,806 (2018)30.5km
Mindat Locality ID:
198161
Long-form identifier:
mindat:1:2:198161:5
GUID (UUID V4):
0


Location: The Iron Creek prospect is on the ridge crest northeast of the head of Ashland Creek, 2.5 miles northeast of the Nome-Teller road. The prospect is at an elevation of about 1,100 feet and near the center of section 6, T. 9 S., R. 35 W., Kateel River Meridian. The location is accurate to within about 500 feet. This is locality 6 of Cobb (1972 [MF 463], 1978 [OFR 78-93]).
Geology: Limonitic rocks occur in a synform near the base of a marble unit (Herreid, 1970, figure 1). According to Mulligan and Hess (1965), samples of outcrop consist of finely crystalline marble with minor disseminated limonite and limonitic cavity fillings; sericitic schist with minor earthy and compacted limonite and accessory rutile is also present. Associated schist consists of chlorite, limonite, quartz, biotite, sericite, manganese oxides (pyrolusite?), and minor clay. There is an estimated resource of 12,000 long tons of material that contains 20 to 40 percent iron and 20,000 long tons of 10 to 20 percent iron (Shallit, 1942; Mulligan and Hess, 1965, table 3). Mulligan and Hess (1965) found no evidence of sulfides at this deposit, and samples collected by Herreid (1970) contained only as much as 220 ppm zinc.
Workings: Some surface prospecting pits are probably present.
Age: Post mid-Cretaceous, the age of metamorphism of the host schist and marble.
Reserves: Shallit (1942; Mulligan and Hess, 1965, table 3) estimated that there are 12,000 long tons of limonitic material containing 20 to 40 percent iron and 20,000 long tons of limonitic material containing 10 to 20 percent iron.

Commodities (Major) - Fe, Mn; (Minor) - Ti
Development Status: None
Deposit Model: Iron oxide veins and replacement of marble and schist.

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


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Pyrolusite4.DB.05Mn4+O2
Rutile4.DB.05TiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Dolomite5.AB.10CaMg(CO3)2
Unclassified
'Limonite'-

List of minerals for each chemical element

CCarbon
C CalciteCaCO3
C DolomiteCaMg(CO3)2
OOxygen
O CalciteCaCO3
O DolomiteCaMg(CO3)2
O PyrolusiteMn4+O2
O RutileTiO2
MgMagnesium
Mg DolomiteCaMg(CO3)2
CaCalcium
Ca CalciteCaCO3
Ca DolomiteCaMg(CO3)2
TiTitanium
Ti RutileTiO2
MnManganese
Mn PyrolusiteMn4+O2

Other Databases

Link to USGS - Alaska:NM131

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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