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Golden Turkey Mine (Silver Pheasant Mine), Turkey Creek, Turkey Creek Mining District, Bradshaw Mountains (Bradshaw Range), Yavapai County, Arizona, USAi
Regional Level Types
Golden Turkey Mine (Silver Pheasant Mine)Mine
Turkey CreekCreek
Turkey Creek Mining DistrictMining District
Bradshaw Mountains (Bradshaw Range)Mountain Range
Yavapai CountyCounty
ArizonaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
34° 16' 10'' North , 112° 12' 16'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Spring Valley1,148 (2011)9.3km
Cordes Lakes2,633 (2011)10.2km
Mayer1,497 (2011)14.5km
Black Canyon City2,837 (2011)22.6km
Dewey-Humboldt3,894 (2011)29.1km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Black Canyon City Rock ClubBlack Canyon City, Arizona23km
Prescott Gem & Mineral ClubPrescott Valley, Arizona39km
Daisy Mountain Rock & Mineral ClubAnthem, Arizona45km
Mindat Locality ID:
48543
Long-form identifier:
mindat:1:2:48543:5
GUID (UUID V4):
3d40fa20-c4d1-40cb-883b-7a6c0e586bf2


A former underground Au-Ag-Pb-Zn-Cu mine located on the West side of Turkey Creek, about 15 miles from Mayer at 3,000 feet of altitude. Discovered 1900 by Theising. Reopened 1933 and owned by H.C. Mitchell & Associates (1934). Produced 1923-1949.

Mineralization is a vein deposit a few inches to more than 1 foot wide with a tabular ore body hosted in the Spud Mountain Volcanics. In places, a branching lode several feet wide. Ore control was faulting and shearing. Ore concentration was oxidation at near surface.

Precambrian schist strikes Northward and dips almost vertically. The vein strikes NE-ward and ranges in dip from 30ΒΊ to less than 10ΒΊ SE. It occupies a fissure zone, probably the result of thrust-faulting. Vein filling consists of a very coarsely-crystalline, milky to clear, glassy quartz with rather abundant, irregular masses and disseminations of sulfides. Vein walls are intensely sericitized and silicified, and in places, contain disseminated metacrysts of practically barren pyrite. The oxidized zone extended to the 250 level on the incline.

Area structures include low-angle (less than 40 degrees) veins that cut across foliation. Foliation and transposed bedding in metavolcanic rocks trends N-S.

Workings include a 100 foot deep shaft; later a 500 foot deep inclined shaft and approximately 2,000 feet of workings.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


6 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
Group 9 - Silicates
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2

List of minerals for each chemical element

HHydrogen
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CCarbon
Cβ“˜ CalciteCaCO3
OOxygen
Oβ“˜ CalciteCaCO3
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
AlAluminium
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ GalenaPbS
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
KPotassium
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ CalciteCaCO3
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
ZnZinc
Znβ“˜ SphaleriteZnS
PbLead
Pbβ“˜ GalenaPbS

Other Regions, Features and Areas containing this locality


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