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Powdermilk Prospect, Kiana Mining District, Northwest Arctic Borough, Alaska, USAi
Regional Level Types
Powdermilk ProspectProspect
Kiana Mining DistrictMining District
Northwest Arctic BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
67° 27' 36'' North , 160° 47' 24'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Kiana361 (2011)56.2km
Mindat Locality ID:
199487
Long-form identifier:
mindat:1:2:199487:5
GUID (UUID V4):
0


Location: The Powdermilk prospect is just southeast of the confluence of the two major headwater forks of a major, unnamed, southeast flowing tributary of the Omar River. Coordinates are for the approximate center of the occurrence. The prospect covers an area of 2 square kilometers. It is in sections 24, 25, T. 24 N., R. 10 W., of the Kateel River Meridian. Schmidt and Allegro (1988), location 157.
Geology: The Powdermilk deposit consists of disseminations and clots (under 2.5 centimeter diameter) of sphalerite, galena, and rare pyrite in Devonian light-gray dolostone (Schmidt and Allegro, 1988). The sphalerite is coarsely crystalline, locally zoned, and medium to dark brown and red. Barite forms veins in the dolostone. Soil samples from the western river bank exposure contain as much as 1600 ppm Pb, 420 ppm Zn and 7.2 ppm Ag. Rock samples from the more oxidized, eastern creek exposure contain as much as 280 ppm Pb, 230 ppm Zn and 21 ppm Ag. Rock samples contain as much as 20% sphalerite, 8% galena and 5% pyrite. The host dolostone strikes NE and dips nearly vertically at the prospect. Synformal structure is suggested. Some gray limestone occurs east of the prospect. The Powdermilk deposit is similar to southeast Missouri Pb-Zn (Cox and Singer, 1986; model 32a) in host rock and mineralization. The sulfides are epigenetic with respect to the host dolostone. Mineralization may be structurally controlled by the synform (Schmidt and Folger, 1986).
Workings: The U.S. Geological Survey did reconnaissance mapping, took 39 soil samples along a sample line, and collected additional rock and pan concentrate samples from the area (Zayatz and others, 1988).
Age: Devonian?
Alteration: Surficial weathering consists of rare iron oxide staining and local clay alteration.

Commodities (Major) - Ag, Pb, Zn; (Minor) - Ba, Cd(?)
Development Status: None
Deposit Model: Southeast Missouri Pb-Zn (Cox and Singer, 1986; model 32a).

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 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4

List of minerals for each chemical element

OOxygen
O BaryteBaSO4
SSulfur
S BaryteBaSO4
S GalenaPbS
S PyriteFeS2
S SphaleriteZnS
FeIron
Fe PyriteFeS2
ZnZinc
Zn SphaleriteZnS
BaBarium
Ba BaryteBaSO4
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:BM010

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.

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