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Black Mountain claims (Black Mountain Vanadium claims; Black Vanadium claim; Ray Vanadium claim), Aguila Mining District, Maricopa County, Arizona, USAi
Regional Level Types
Black Mountain claims (Black Mountain Vanadium claims; Black Vanadium claim; Ray Vanadium claim)Group of Claims
Aguila Mining DistrictMining District
Maricopa CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
33° 51' 24'' North , 113° 3' 14'' West
Latitude & Longitude (decimal):
Type:
Group of Claims
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Aguila798 (2011)14.6km
Wickenburg6,806 (2017)32.4km
Congress1,975 (2014)38.8km
Morristown227 (2017)39.7km
Wenden728 (2011)45.2km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Wickenburg Gem and Mineral SocietyWickenburg, Arizona32km
Mindat Locality ID:
44148
Long-form identifier:
mindat:1:2:44148:6
GUID (UUID V4):
81cf4a64-d088-40c8-830b-d417e9a73236


‡Ref.: Granger, H.C. & R.B. Raup (1962), Recon. study of uranium deposits in AZ, USGS Bull. 1147-A: A15; Hewett, D.F. (1925), Carnotite discovered near Aguila, AZ, Engr.Mining Jour.: 120: 19; Scarborough, Robert B. (1981), Radioactive occurrences and uranium production in Arizona, prepared for US Dept. of Energy; AZ Dept. Min. Resources (ADMR) "U" file; USGS 15 minute Aguila topo. map; Flagg, F.L., Vanadium Rept. Book I; MRDS files #10027055 & 10234892.

A group of U claims located on the West end of the Vulture Mountains, about 12 miles SE of Aguila. Owned by Mr. Milton Ray of Aguila (1951).

Mineralization is uranium deposits in shaly beds of buff to white, limy bentonitic tuff, from 100 to 200 feet thick. The tuff is exposed along a northwest-trending cuesta that is capped by a mafic lava flow. Underlying the tuff are gneiss and schist cut by pegmatite dikes. The tuff beds strike NW & dip 60º to 65º SW; the steeper dips are caused by slumping. Bedding planes and fracture surfaces are thinly coated with gypsum and a yellow uranium mineral, probably carnotite. Host rock units are the Coconino, Hermit & Supai formations; Redwall limestone.

Workings include shallow prospect pits and trenches.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


2 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Carnotite4.HB.05K2(UO2)2(VO4)2 · 3H2O
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Gypsum7.CD.40CaSO4 · 2H2O

List of minerals for each chemical element

HHydrogen
H CarnotiteK2(UO2)2(VO4)2 · 3H2O
H GypsumCaSO4 · 2H2O
OOxygen
O CarnotiteK2(UO2)2(VO4)2 · 3H2O
O GypsumCaSO4 · 2H2O
SSulfur
S GypsumCaSO4 · 2H2O
KPotassium
K CarnotiteK2(UO2)2(VO4)2 · 3H2O
CaCalcium
Ca GypsumCaSO4 · 2H2O
VVanadium
V CarnotiteK2(UO2)2(VO4)2 · 3H2O
UUranium
U CarnotiteK2(UO2)2(VO4)2 · 3H2O

Other Regions, Features and Areas containing this locality

North America PlateTectonic Plate
USA

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