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Tolstoi Creek Prospect (ARDF - ID007), Innoko Mining District, Yukon-Koyukuk Census Area, Alaska, USAi
Regional Level Types
Tolstoi Creek Prospect (ARDF - ID007)Prospect
Innoko Mining DistrictMining District
Yukon-Koyukuk Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
62° 58' 57'' North , 156° 59' 49'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Mindat Locality ID:
200385
Long-form identifier:
mindat:1:2:200385:9
GUID (UUID V4):
7683a2de-726d-431b-b2f0-5fee09c91119


Location: This prospect at an elevation of about 1,400 feet on an unnamed tributary of Tolstoi Creek. It is about 1.0 mile north of hill 2008 and about 0.4 mile southwest of the northeast corner of section 2, T. 33 N., R. 41 W., of the Seward Meridian. The location is accurate.
Geology: The Tolstoi Creek prospect is a black-sand-rich gold placer that contains visible gold, abundant magnetite, ilmenite, less abundant ilmenorutile, a Nb-Ta mineral, cinnabar, tourmaline (variety dravite), and a trace of chalcopyrite (Bundtzen, Cox and Veach, 1987). The creek is about 30 feet wide and is incised in glacial moraine of late Pleistocene age. The alluvium is poorly sorted; most of the gold and heavy minerals occur in sand and gravel that is interstitial to erratic boulders that originated in the Beaver Mountains (Bundtzen and Laird, 1980). The placer gold is mostly fine-grained with occasional grains to 5 mm across. Six pans collected at intervals across the creek contained from 1 to 5 grains of gold per pan (Bundtzen, Cox and Veach, 1987). The average fineness of the placer gold as determined by fire assay is 891. One placer concentrate contained 214 parts per million (ppm) niobium 14 ppm tantalum, 8.1 ppm gold, and 1.0 ppm silver (Bundtzen, Cox, and Veach, 1987).
Workings: Placer occurrences in this area were prospected during the early part of the 20th century (Mertie, 1936). The placer was sampled by the Alaska Division of Geological and Geophysical Surveys in the 1980s (Bundtzen, Cox, and Veach, 1987).
Age: The prospect is in reworked, glacial moraine of Late Pleistocene (Wisconsin?) age and the placer is either late Pleistocene or Holocene in age (Bundtzen, 1980 [GR 63]).
Alteration: None.
Production: No known production.

Commodities (Major) - Au; (Minor) - Cu, Hg, Nb, Ta
Development Status: None
Deposit Model: Placer Au deposit (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


7 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Cinnabar2.CD.15aHgS
Group 4 - Oxides and Hydroxides
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Ilmenite4.CB.05Fe2+TiO3
β“˜Rutile
var. Ilmenorutile
4.DB.05(Ti,Nb)O2
β“˜4.DB.05TiO2
Group 9 - Silicates
β“˜Dravite9.CK.05NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Unclassified
β“˜'Tourmaline'-AD3G6 (T6O18)(BO3)3X3Z

List of minerals for each chemical element

HHydrogen
Hβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
BBoron
Bβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
OOxygen
Oβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ Rutile var. Ilmenorutile(Ti,Nb)O2
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ RutileTiO2
Oβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
NaSodium
Naβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
MgMagnesium
Mgβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
AlAluminium
Alβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
SiSilicon
Siβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ CinnabarHgS
TiTitanium
Tiβ“˜ IlmeniteFe2+TiO3
Tiβ“˜ Rutile var. Ilmenorutile(Ti,Nb)O2
Tiβ“˜ RutileTiO2
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ IlmeniteFe2+TiO3
Feβ“˜ MagnetiteFe2+Fe23+O4
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
NbNiobium
Nbβ“˜ Rutile var. Ilmenorutile(Ti,Nb)O2
AuGold
Auβ“˜ GoldAu
HgMercury
Hgβ“˜ CinnabarHgS

Other Databases

Link to USGS - Alaska:ID007

Other Regions, Features and Areas containing this locality


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