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Kit Carson Mine (Kit Carson vein; Kit Carson and Walter prospect), Agua Fria Mining District, Bradshaw Mountains (Bradshaw Range), Yavapai County, Arizona, USAi
Regional Level Types
Kit Carson Mine (Kit Carson vein; Kit Carson and Walter prospect)Mine
Agua Fria Mining DistrictMining District
Bradshaw Mountains (Bradshaw Range)Mountain Range
Yavapai CountyCounty
ArizonaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
34° 29' 39'' North , 112° 16' 27'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Dewey-Humboldt3,894 (2011)5.0km
Mayer1,497 (2011)11.3km
Prescott Valley42,197 (2017)13.4km
Prescott41,899 (2017)18.5km
Spring Valley1,148 (2011)19.7km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Prescott Gem & Mineral ClubPrescott Valley, Arizona13km
Mingus Gem & Mineral ClubCottonwood, Arizona36km
Verde River RockhoundsCottonwood, Arizona36km
Black Canyon City Rock ClubBlack Canyon City, Arizona48km
Mindat Locality ID:
50981
Long-form identifier:
mindat:1:2:50981:4
GUID (UUID V4):
d6228524-f481-4bf6-8388-65999fea1e18


A former Ag-Au-Cu-Pb mine on the Kit Carson vein, which is located about 1,500 feet west of the Silver Belt-McCabe vein. Discovered in 1897. Produced 1907-1926.

The Kit Carson vein strikes parallel to the Silver Belt-McCabe vein, but has an opposite dip to the east and is hosted in the Lower Unit of the Spud Mountain Volcanics. The Kit Carson vein was traced on the surface for about 4,000 feet, but is somewhat longer, for its northern extent is overlain by the gravel of the Hickey formation in Lonesome Valley. Little is known about this vein. It appears to resemble the Silver Belt-McCabe vein in structure, alteration, and character of the mineralized zone.

The vein consists of a sheared zone as much as 5 feet wide, characterized by fissile, sericitic rock in which local stringers of comb quartz and boxwork, possibly after ankerite, were observed. Mineralization is a 2 to 4 foot wide vein with well-defined wall rock. Ore control was faulting and shearing. Ore concentration was oxidation at near surface. Alteration was minor silicification. The Kit Carson vein is West of the Silver Belt-McCabe vein and dips N.30ΒΊE. and dips steeply SE.

Area structures include veins that parallel regional foliation, which trends N30E.

Workings include 8 shafts and prospect pits.

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 1 - Elements
β“˜Silver1.AA.05Ag
Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Pyrite2.EB.05aFeS2
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Vanadinite8.BN.05Pb5(VO4)3Cl

List of minerals for each chemical element

CCarbon
Cβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
OOxygen
Oβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Oβ“˜ QuartzSiO2
Oβ“˜ VanadinitePb5(VO4)3Cl
MgMagnesium
Mgβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
SiSilicon
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ PyriteFeS2
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ClChlorine
Clβ“˜ VanadinitePb5(VO4)3Cl
CaCalcium
Caβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
VVanadium
Vβ“˜ VanadinitePb5(VO4)3Cl
FeIron
Feβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
AgSilver
Agβ“˜ SilverAg
SbAntimony
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
PbLead
Pbβ“˜ VanadinitePb5(VO4)3Cl

Other Databases

Link to USGS MRDS:10048073

Other Regions, Features and Areas containing this locality


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References

 
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