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Tiglukpuk Creek Occurrence, Colville Mining District, North Slope Borough, Alaska, USAi
Regional Level Types
Tiglukpuk Creek OccurrenceOccurrence
Colville Mining DistrictMining District
North Slope BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
68° 18' 0'' North , 151° 53' 24'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Anaktuvuk Pass337 (2017)18.5km
Mindat Locality ID:
200355
Long-form identifier:
mindat:1:2:200355:2
GUID (UUID V4):
0


Location: Deposits on a small tributary of Skimo Creek and on Tiglukpuk Creek. Within one mile.
Geology: Phosphate deposits restricted to black chert and shale unit of the Alapha Limestone of late Mississippian age. Phosphate rock and phosphorites occur within a section of interbedded oolitic to pisolitic limestone, chert, and shale. Marked variation in lithologic character of phosphate content. Fluorite was a constituent of all samples studied.
Workings: A 36 ft thick sequence averages 8% P2O5; a 43 in. thick sequence averages 21% P2O5; and 6 beds, none more than 5.5 in. thick, contain 30% P2O5. Samples analyzed for vanadium contained .04% - .10% V2O5. Samples collected by USBM contained up to 23% phosphate with 1035 ppm V.
Age: Mississippian

Commodities (Major) - P; (Minor) - V
Development Status: No
Deposit Model: Bedded phosphorite

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


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 8 - Phosphates, Arsenates and Vanadates
Fluorapatite8.BN.05Ca5(PO4)3F

List of minerals for each chemical element

OOxygen
O FluorapatiteCa5(PO4)3F
FFluorine
F FluorapatiteCa5(PO4)3F
PPhosphorus
P FluorapatiteCa5(PO4)3F
CaCalcium
Ca FluorapatiteCa5(PO4)3F

Other Databases

Link to USGS - Alaska:CL002

Other Regions, Features and Areas containing this locality


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References

 
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