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Verde Central Mine (Verde King Mine), Deception Gulch, Jerome, Verde Mining District, Black Hills (Black Hill Range), Yavapai County, Arizona, USAi
Regional Level Types
Verde Central Mine (Verde King Mine)Mine
Deception GulchGulch
JeromeTown
Verde Mining DistrictMining District
Black Hills (Black Hill Range)Group of Hills
Yavapai CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
34° 44' 24'' North , 112° 7' 15'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Jerome456 (2017)1.2km
Clarkdale4,240 (2017)6.7km
Cottonwood11,818 (2017)10.2km
Verde Village11,605 (2011)10.5km
Cornville3,280 (2011)18.4km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Mingus Gem & Mineral ClubCottonwood, Arizona10km
Verde River RockhoundsCottonwood, Arizona10km
Prescott Gem & Mineral ClubPrescott Valley, Arizona23km
Sedona Gem & Mineral ClubSedona, Arizona36km
Mindat Locality ID:
40916
Long-form identifier:
mindat:1:2:40916:1
GUID (UUID V4):
0


A former underground Cu-Ag-Au mine located on 20 claims in upper Deception Gulch, about 4,000 feet south of the United Verde Mine, and about 1 mile SW of Jerome. Owned by the Verde Central Mines, Inc.; and then, Phelps Dodge Corp. Closed in 1929.

Mineralization is a vein deposit with a tabular orebody hosted in the Deception Rhyolite, Cleopatra Quartz Porphyry and an unknown metabasalt. Ore control was stratigraphy and igneous activity. Ore concentration was oxidation at near surface. Alteration was chloritization and sericitization.

The Verde Central ore zone is along the east margin of the quartz porphyry in contact with the Deception Rhyolite. The contact is irregular and interfingering, and dike offshoots of porphyry cut the rhyolite. The Verde Central was a blind prospect. Two ore bodies were found.

Mineralization is a fault vein with bunches of quartz and local copper staining. The country rock is greenstone with intrusive tongues of quartz porphyry, both more or less schistose and difficult to separate. The vein strikes N.40º-60ºW. and dips 60ºNE. Schistosity strikes N.20ºW. In places there is much disseminated ore through 15 to 20 feet of schist, with copper content of 1 to 3%.

Area structures include foliation in metavolcanic rocks that trends N10W to N40W. Massive sulfide lenses elongate parallel to bedding in metavolcanic rocks.

Workings include a 60º inclined shaft about 800 feet deep on the incline that connects with 4 levels of workings aggregating 2,000 feet. A 1,900 foot deep shaft was ultimately sunk. A long crosscut was driven to the west on the 1450 level.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


3 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
Group 9 - Silicates
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
H MuscoviteKAl2(AlSi3O10)(OH)2
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
OOxygen
O MuscoviteKAl2(AlSi3O10)(OH)2
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
AlAluminium
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
S ChalcopyriteCuFeS2
S PyriteFeS2
KPotassium
K MuscoviteKAl2(AlSi3O10)(OH)2
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2

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