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Copper King Mine (Lawler Mines), Bagdad, Eureka Mining District, Yavapai County, Arizona, USAi
Regional Level Types
Copper King Mine (Lawler Mines)Mine
Bagdad- not defined -
Eureka Mining DistrictMining District
Yavapai CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
34° 34' 10'' North , 113° 13' 44'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Bagdad1,876 (2016)2.6km
Wikieup133 (2011)38.0km
Congress1,975 (2014)57.0km
Yarnell649 (2011)58.7km
Mindat Locality ID:
61212
Long-form identifier:
mindat:1:2:61212:7
GUID (UUID V4):
c32d29f6-b66b-4cba-9164-ea47a68dfeea


A former underground Zn-Pb-Cu-Ag-Au mine located on one patented claim 1Β½ miles south of Bagdad. Located January 1, 1881 by William Waters. Relocated on March 28, 1891 by Fred Maroney and John Lawler and patented by them May 1, 1893. Arizona Hillside Development Co. obtained an option on the claim and acquired surrounding claims (circa 1917). World Exploration Co. obtained control in 1925- 1927. Ownership reverted to John Lawler's heirs, M.L. Lynch & J.W. Lawler. Valerio Rossi leased it during WWII. Goodwin Mining Co. purchased it in 1948. Owned by E.A. Scholz & J.H. Cazier (1950 - circa 1955). Produced 1917-1957.

One of two known examples of massive-sulfide replacement deposits in the Bagdad area. The sulfides have replaced rocks of the Bridle formation near a mass of King Peak rhyolite.

The ore is localized in a unit of tuffaceous sedimentary rock near massive lavas of the Bridle formation. The ore appears as massive-sulfide lenses from 2 to 10 feet (60 cm to 9 meters) wide, and from 10 to 120 feet long, and as much as 100 feet deep, and lies in a broad northeast-trending zone of minor faults. The ore is localized along interlacing small faults and along rolls in the bedding of the tuffaceous sedimentary rocks which strike NE, and are overturned and dip 45ΒΊ to 55ΒΊNW. The ore zone is essentially parallel to the bedding and zone of minor faults. Oxidation and enrichment to 30 feet deep.

The bleached, sericitized and silicified zone in the Bridle formation is of limited width, ranging only from several inches to 3 feet along the solution channels. Alteration also includes chloritization and pyritization.

The ore consists of massive granular, brown, resinous sphalerite in association with smaller quantities of Cu & Pb sulfides. Two major lenses of ore, one north and one south of the inclined shaft, center about 100 level, and a third major lens, south of the shaft centers about the 300 level.

Workings include 9 irregularly spaced levels and a total of more than 4,000 feet of workings. An inclined shaft is sunk to the lowest level (600). The ore averaged 46.89% Zn, 5.7 oz. Ag/T, 3.58% Pb and 1.68% Cu. Total production (1917-1951) was 120 oz. Au, 77,376 oz. Ag, 542,794 pounds Cu, 935,459 pounds Pb and 13,466,268 pounds of Zn.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


24 valid minerals.

Detailed Mineral List:

β“˜ Anglesite
Formula: PbSO4
β“˜ Azurite
Formula: Cu3(CO3)2(OH)2
β“˜ Calcite
Formula: CaCO3
β“˜ Cerussite
Formula: PbCO3
β“˜ Chalcanthite
Formula: CuSO4 · 5H2O
Description: Coatings on walls of drifts.
β“˜ Chalcocite
Formula: Cu2S
Description: Small quantities; partly replaces sphalerite and chalcopyrite.
β“˜ Chalcopyrite
Formula: CuFeS2
β“˜ 'Chlorite Group'
β“˜ Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
β“˜ Conichalcite
Formula: CaCu(AsO4)(OH)
Colour: Green
Description: As radiating fibrous coatings on oxidized ore.
β“˜ Copper
Formula: Cu
β“˜ Covellite
Formula: CuS
Description: Partly replaces chalcopyrite and sphalerite.
β“˜ Cuprite
Formula: Cu2O
β“˜ Galena
Formula: PbS
β“˜ Goslarite
Formula: ZnSO4 · 7H2O
Description: Found in upper workings; seasonally (summer) it coats the dump making it visible from a distance.
β“˜ Gypsum
Formula: CaSO4 · 2H2O
Habit: To 2 inches (5 cm) long
Colour: Colorless
Description: Crystals embedded in oxidized ore.
β“˜ Gypsum var. Selenite
Formula: CaSO4 · 2H2O
Habit: To 2 inches (5 cm) long
Colour: Colorless
Description: Crystals embedded in oxidized ore.
β“˜ Hematite
Formula: Fe2O3
Description: Occurs locally along the margins and ends of the ore lenses and a large mass outcrops at the surface on the footwall side of the ore zone.
β“˜ Hematite var. Specularite
Formula: Fe2O3
βœͺ Hemimorphite
Formula: Zn4Si2O7(OH)2 · H2O
Habit: Beautiful prismatic crystals
Colour: Colorless
Description: Crystals and botryoidal crusts in the oxidized zone; common constituent of the oxidized zinc ore.
β“˜ 'Limonite'
Colour: Reddish
Description: Cellular to fluffy in the oxidized zone, usually adjacent to or above the massive sulfide lenses.
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
Description: Occurs along the margins and ends of the massive sulphide lenses.
β“˜ Malachite
Formula: Cu2(CO3)(OH)2
Description: Common.
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Pyrite
Formula: FeS2
β“˜ Quartz
Formula: SiO2
Description: Rarely appearing as minute crystals in vugs.
β“˜ Smithsonite
Formula: ZnCO3
Description: Earthy; a common constituent of the oxidized zinc ore.
β“˜ Smithsonite var. Dry Bone Ore
Formula: ZnCO3
Description: Earthy; a common constituent of the oxidized zinc ore.
β“˜ Sphalerite
Formula: ZnS
Description: Granular, massive replacement ore.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Copper1.AA.05Cu
Group 2 - Sulphides and Sulfosalts
β“˜Chalcocite2.BA.05Cu2S
β“˜Covellite2.CA.05aCuS
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
β“˜Cuprite4.AA.10Cu2O
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Hematite4.CB.05Fe2O3
β“˜var. Specularite4.CB.05Fe2O3
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Smithsonite
var. Dry Bone Ore
5.AB.05ZnCO3
β“˜5.AB.05ZnCO3
β“˜Calcite5.AB.05CaCO3
β“˜Cerussite5.AB.15PbCO3
β“˜Azurite5.BA.05Cu3(CO3)2(OH)2
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Anglesite7.AD.35PbSO4
β“˜Chalcanthite7.CB.20CuSO4 Β· 5H2O
β“˜Goslarite7.CB.40ZnSO4 Β· 7H2O
β“˜Gypsum
var. Selenite
7.CD.40CaSO4 Β· 2H2O
β“˜7.CD.40CaSO4 Β· 2H2O
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Conichalcite8.BH.35CaCu(AsO4)(OH)
Group 9 - Silicates
β“˜Hemimorphite9.BD.10Zn4Si2O7(OH)2 Β· H2O
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1
Unclassified
β“˜'Limonite'-
β“˜'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ AzuriteCu3(CO3)2(OH)2
Hβ“˜ ChalcanthiteCuSO4 · 5H2O
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ ConichalciteCaCu(AsO4)(OH)
Hβ“˜ GoslariteZnSO4 · 7H2O
Hβ“˜ GypsumCaSO4 · 2H2O
Hβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ Gypsum var. SeleniteCaSO4 · 2H2O
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CCarbon
Cβ“˜ AzuriteCu3(CO3)2(OH)2
Cβ“˜ CalciteCaCO3
Cβ“˜ CerussitePbCO3
Cβ“˜ MalachiteCu2(CO3)(OH)2
Cβ“˜ SmithsoniteZnCO3
Cβ“˜ Smithsonite var. Dry Bone OreZnCO3
OOxygen
Oβ“˜ AnglesitePbSO4
Oβ“˜ AzuriteCu3(CO3)2(OH)2
Oβ“˜ CalciteCaCO3
Oβ“˜ CerussitePbCO3
Oβ“˜ ChalcanthiteCuSO4 · 5H2O
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ ConichalciteCaCu(AsO4)(OH)
Oβ“˜ CupriteCu2O
Oβ“˜ GoslariteZnSO4 · 7H2O
Oβ“˜ GypsumCaSO4 · 2H2O
Oβ“˜ HematiteFe2O3
Oβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ QuartzSiO2
Oβ“˜ SmithsoniteZnCO3
Oβ“˜ Gypsum var. SeleniteCaSO4 · 2H2O
Oβ“˜ Hematite var. SpeculariteFe2O3
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oβ“˜ Smithsonite var. Dry Bone OreZnCO3
AlAluminium
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ QuartzSiO2
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SSulfur
Sβ“˜ AnglesitePbSO4
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ ChalcanthiteCuSO4 · 5H2O
Sβ“˜ ChalcociteCu2S
Sβ“˜ CovelliteCuS
Sβ“˜ GalenaPbS
Sβ“˜ GoslariteZnSO4 · 7H2O
Sβ“˜ GypsumCaSO4 · 2H2O
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
Sβ“˜ Gypsum var. SeleniteCaSO4 · 2H2O
KPotassium
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ CalciteCaCO3
Caβ“˜ ConichalciteCaCu(AsO4)(OH)
Caβ“˜ GypsumCaSO4 · 2H2O
Caβ“˜ Gypsum var. SeleniteCaSO4 · 2H2O
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ HematiteFe2O3
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ PyriteFeS2
Feβ“˜ Hematite var. SpeculariteFe2O3
CuCopper
Cuβ“˜ AzuriteCu3(CO3)2(OH)2
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChalcanthiteCuSO4 · 5H2O
Cuβ“˜ ChalcociteCu2S
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ ConichalciteCaCu(AsO4)(OH)
Cuβ“˜ CovelliteCuS
Cuβ“˜ CupriteCu2O
Cuβ“˜ CopperCu
Cuβ“˜ MalachiteCu2(CO3)(OH)2
ZnZinc
Znβ“˜ GoslariteZnSO4 · 7H2O
Znβ“˜ HemimorphiteZn4Si2O7(OH)2 · H2O
Znβ“˜ SmithsoniteZnCO3
Znβ“˜ SphaleriteZnS
Znβ“˜ Smithsonite var. Dry Bone OreZnCO3
AsArsenic
Asβ“˜ ConichalciteCaCu(AsO4)(OH)
PbLead
Pbβ“˜ AnglesitePbSO4
Pbβ“˜ CerussitePbCO3
Pbβ“˜ GalenaPbS

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