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Safford deposit (Spalding; Lindsey and Anderson claims; Sanchez Copper deposit; Esperanza Mine), Sanchez, Lone Star Mining District (Safford Mining District; Dos Pobres Mining District), Graham County, Arizona, USAi
Regional Level Types
Safford deposit (Spalding; Lindsey and Anderson claims; Sanchez Copper deposit; Esperanza Mine)Deposit
Sanchez- not defined -
Lone Star Mining District (Safford Mining District; Dos Pobres Mining District)Mining District
Graham CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
32° 52' 53'' North , 109° 32' 2'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
San Jose506 (2011)8.7km
Solomon426 (2011)12.1km
Safford9,683 (2017)17.1km
Thatcher4,992 (2017)21.3km
Cactus Flat1,518 (2011)21.8km
Mindat Locality ID:
53634
Long-form identifier:
mindat:1:2:53634:0
GUID (UUID V4):
00c04dd9-ffdc-4f48-9d1b-babe280f0e46


An underground Cu-Au mine located in secs. 25 & 26, T6S, R27E, 9 miles ENE of Safford, at Sanchez, on BLM-administered land. Lat-long is for approximate central point of the mineralized area - the old shaft in sec. 26 is at 32-52-57N, 109-32-43W; the prospect in sec. 25 is at 32-52-53N, 109-32-02W. Discovered 1899. Produced 1899 to the late 1930's. Owned and operated by the Azco Mining Inc., Lakewood, CO (1988). Also known as / designated: Maravilla Copper Co.; Lone Wolf shaft; Lead Hill; Kirtland Hill group; Iron King; Consolidated Metals MS 4590 claim; Clara; Bear Creek; United Nuclear; Nancy group; Arichise Copper Co.; Bellmon; Bob Carresco; Carpenter; Esperanza Sanchez; AZCO Minintg Inc. project; Kennecott Safford Mine; Carpenter Mine; Safford Inspiration Mine; and McBride. Unpatented mining claims extend into secs. 13-16 & 18-24, 26-28, and 34-36; and secs. 23-36, T5S, R26E.

Mineralization is a pipe-shaped porphyry copper deposit hosted in Safford Volcanics and breccia that is 762 meters long and 762 meters wide and 1066.8 meters thick, hosted in volcanic agglomerate and andesite. Ore centered on oldest of four monzonite porphyry intrusive phases but mostly hosted by andesite. Associated rock unit is the Lone Star pluton (monzonite). Concentration was hydrothermal and oxidation. Ore control was NE-trending shears intruded by dikes. Ore concentration was shearing and fracturing of older andesites, followed by intrusion of later igneous plugs and porphyries alogn shear zones. Shearing and fracturing continued, followed by alteration and iron and copper sulfide mineralization. The deposit later was enriched by formation of a chalcocite enrichment blanket. It was subsequently covered by volcanics. NW block faulting uplifted and tilted the Gila Mountains and further oxidized the deposit.

Alteration involves four hypogene alteration zones: 1) Sericitization & silicification in rhyolite, latite, and quartz latite; 2) Biotization in andesite; 3) Chloritization; and 4) Propylitic alteration. The ore body is in zones 1 & 2. Supergene enrichment has taken place to average dept of 440 feet.

Quartz monzonite is associated with the mineralization. The ore grade is highest in the main stock. The oxide zone extends to 1050 feet depth. Mixed oxide/native copper zone from 1050 to 1200 feet depth, sulfide below 1200 feet depth. A small chalcocite enrichment blanket formed in the breccia pipe but was later oxidized. The oxide zone consists of coatings of chrysocolla, neotocite, tenorite, minor native copper, and trace atacamite on fractures accompanied by goethite, minor hematite, and rare jarosite. Chrysocolla also occurs as disseminations in plagioclase. The mixed zone consists of Chrysocolla, neotocite, native copper, delafossite, cuprite (?), chalcopyrite, bornite, and minor molybdenite. The original total sulfide content averaged 1.5 vol. % with up to 5 vol. % in the breccia pipe. Protore grade was about 0.3% Cu.

Area structures include the Lone Star shear zone 6000 feet wide and 16000 feet long that strikes N50Β°-65Β°E, steep to vertical dip.

Workings include a shaft sunk by Carpenter on oxide Cu ore outcrop about 1910. Porphyry Cu potential recognized by Bear Creek Mining Co. (Kennecott) in the 1950's. The first hole cut about 1000 feet of 1% Cu. Subsequently explored bys several uranium, oil and mining companies of which Inspiration did the most work. Inspiration (late 1960's to early 1970's) identified sulphide copper mineralization below the oxide zone, but Azco was not pursuing the sulphide mineralization in 1989. In 1993, BLM approved the project after Azco completed a full environmental impact statement process. A total of 150 holes have been drilled with 190,000 feet of total footage.

Reserves amount to ore for at least 20 years of operation. Reserve-Resources: within the 250,000,000 st oxide reserve (1988) is an open pit minable block of 120,000,000 st at a grade of 0.37% Cu. Proposed open pit-heap leach operation. Development was to have begun in 1995. Plans to leach 100,000 to 150,000 tons/week.

Production: about 50,000 st bulk samples mined from open pits by Inspiration from 1969 to 1972. Azco mined additional bulk samples from the same pits.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


31 valid minerals.

Detailed Mineral List:

β“˜ Alunite
Formula: KAl3(SO4)2(OH)6
β“˜ Antlerite
Formula: Cu3(SO4)(OH)4
β“˜ Atacamite
Formula: Cu2(OH)3Cl
β“˜ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
β“˜ Bornite
Formula: Cu5FeS4
Description: In veins and as disseminations.
β“˜ Brochantite
Formula: Cu4(SO4)(OH)6
β“˜ Calcite
Formula: CaCO3
β“˜ Chalcanthite
Formula: CuSO4 · 5H2O
β“˜ Chalcocite
Formula: Cu2S
Description: Steely & sooty varieties replacing pyrite, chalcopyrite & bornite; blanket-like enrichment cap on primary ore zone.
β“˜ Chalcopyrite
Formula: CuFeS2
β“˜ 'Chlorite Group'
β“˜ Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Description: Most abundant copper mineral as veins, blebs & coatings.
β“˜ Copper
Formula: Cu
Description: Along thin veinlets or fractures in oxidized zone.
β“˜ Covellite
Formula: CuS
β“˜ Cuprite
Formula: Cu2O
Description: Occurs in the oxidized zone.
β“˜ Cuprite var. Chalcotrichite
Formula: Cu2O
Description: Occurs in the oxidized zone.
β“˜ Delafossite
Formula: CuFeO2
β“˜ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜ Galena
Formula: PbS
β“˜ Goethite
Formula: Ξ±-Fe3+O(OH)
β“˜ Gold
Formula: Au
β“˜ Halloysite
Formula: Al2(Si2O5)(OH)4
β“˜ Hematite
Formula: Fe2O3
β“˜ Jarosite
Formula: KFe3+3(SO4)2(OH)6
Description: Occurs in the oxidized zone of the deposit in fractures & veins as a replacement of primary minerals, fault gouge & clay.
β“˜ Kaolinite
Formula: Al2(Si2O5)(OH)4
β“˜ 'Limonite'
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
β“˜ Malachite
Formula: Cu2(CO3)(OH)2
β“˜ Molybdenite
Formula: MoS2
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Neotocite
Formula: (Mn,Fe,Mg)SiO3 · H2O
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
β“˜ Pyrite
Formula: FeS2
Description: Primary sulfide mineral.
β“˜ Sphalerite
Formula: ZnS
β“˜ Tenorite
Formula: CuO
β“˜ 'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
β“˜ Turquoise
Formula: CuAl6(PO4)4(OH)8 · 4H2O
Description: Intimately associated with other phosphates.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Copper1.AA.05Cu
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
β“˜Chalcocite2.BA.05Cu2S
β“˜Bornite2.BA.15Cu5FeS4
β“˜Covellite2.CA.05aCuS
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Molybdenite2.EA.30MoS2
β“˜Pyrite2.EB.05aFeS2
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 3 - Halides
β“˜Atacamite3.DA.10aCu2(OH)3Cl
Group 4 - Oxides and Hydroxides
β“˜Goethite4.00.Ξ±-Fe3+O(OH)
β“˜Cuprite4.AA.10Cu2O
β“˜var. Chalcotrichite4.AA.10Cu2O
β“˜Tenorite4.AB.10CuO
β“˜Delafossite4.AB.15CuFeO2
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Hematite4.CB.05Fe2O3
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Antlerite7.BB.15Cu3(SO4)(OH)4
β“˜Brochantite7.BB.25Cu4(SO4)(OH)6
β“˜Alunite7.BC.10KAl3(SO4)2(OH)6
β“˜Jarosite7.BC.10KFe3+3(SO4)2(OH)6
β“˜Chalcanthite7.CB.20CuSO4 Β· 5H2O
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Turquoise8.DD.15CuAl6(PO4)4(OH)8 Β· 4H2O
Group 9 - Silicates
β“˜Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Kaolinite9.ED.05Al2(Si2O5)(OH)4
β“˜Halloysite9.ED.10Al2(Si2O5)(OH)4
β“˜Neotocite9.ED.20(Mn,Fe,Mg)SiO3 Β· H2O
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1
Unclassified
β“˜'Limonite'-
β“˜'Chlorite Group'-
β“˜'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8

List of minerals for each chemical element

HHydrogen
Hβ“˜ AluniteKAl3(SO4)2(OH)6
Hβ“˜ AntleriteCu3(SO4)(OH)4
Hβ“˜ AtacamiteCu2(OH)3Cl
Hβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hβ“˜ BrochantiteCu4(SO4)(OH)6
Hβ“˜ ChalcanthiteCuSO4 · 5H2O
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hβ“˜ GoethiteΞ±-Fe3+O(OH)
Hβ“˜ HalloysiteAl2(Si2O5)(OH)4
Hβ“˜ JarositeKFe33+(SO4)2(OH)6
Hβ“˜ KaoliniteAl2(Si2O5)(OH)4
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ Neotocite(Mn,Fe,Mg)SiO3 · H2O
Hβ“˜ TurquoiseCuAl6(PO4)4(OH)8 · 4H2O
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CCarbon
Cβ“˜ CalciteCaCO3
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ AluniteKAl3(SO4)2(OH)6
Oβ“˜ AntleriteCu3(SO4)(OH)4
Oβ“˜ AtacamiteCu2(OH)3Cl
Oβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oβ“˜ BrochantiteCu4(SO4)(OH)6
Oβ“˜ CalciteCaCO3
Oβ“˜ ChalcanthiteCuSO4 · 5H2O
Oβ“˜ Cuprite var. ChalcotrichiteCu2O
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ CupriteCu2O
Oβ“˜ DelafossiteCuFeO2
Oβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oβ“˜ GoethiteΞ±-Fe3+O(OH)
Oβ“˜ HalloysiteAl2(Si2O5)(OH)4
Oβ“˜ HematiteFe2O3
Oβ“˜ JarositeKFe33+(SO4)2(OH)6
Oβ“˜ KaoliniteAl2(Si2O5)(OH)4
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ Neotocite(Mn,Fe,Mg)SiO3 · H2O
Oβ“˜ TenoriteCuO
Oβ“˜ TurquoiseCuAl6(PO4)4(OH)8 · 4H2O
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
FFluorine
Fβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
NaSodium
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mgβ“˜ Neotocite(Mn,Fe,Mg)SiO3 · H2O
AlAluminium
Alβ“˜ AluniteKAl3(SO4)2(OH)6
Alβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Alβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alβ“˜ HalloysiteAl2(Si2O5)(OH)4
Alβ“˜ KaoliniteAl2(Si2O5)(OH)4
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ TurquoiseCuAl6(PO4)4(OH)8 · 4H2O
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siβ“˜ HalloysiteAl2(Si2O5)(OH)4
Siβ“˜ KaoliniteAl2(Si2O5)(OH)4
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ Neotocite(Mn,Fe,Mg)SiO3 · H2O
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pβ“˜ TurquoiseCuAl6(PO4)4(OH)8 · 4H2O
SSulfur
Sβ“˜ AluniteKAl3(SO4)2(OH)6
Sβ“˜ AntleriteCu3(SO4)(OH)4
Sβ“˜ BorniteCu5FeS4
Sβ“˜ BrochantiteCu4(SO4)(OH)6
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ ChalcanthiteCuSO4 · 5H2O
Sβ“˜ ChalcociteCu2S
Sβ“˜ CovelliteCuS
Sβ“˜ GalenaPbS
Sβ“˜ JarositeKFe33+(SO4)2(OH)6
Sβ“˜ MolybdeniteMoS2
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ClChlorine
Clβ“˜ AtacamiteCu2(OH)3Cl
KPotassium
Kβ“˜ AluniteKAl3(SO4)2(OH)6
Kβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kβ“˜ JarositeKFe33+(SO4)2(OH)6
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ CalciteCaCO3
Caβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MnManganese
Mnβ“˜ Neotocite(Mn,Fe,Mg)SiO3 · H2O
FeIron
Feβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Feβ“˜ BorniteCu5FeS4
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ DelafossiteCuFeO2
Feβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feβ“˜ GoethiteΞ±-Fe3+O(OH)
Feβ“˜ HematiteFe2O3
Feβ“˜ JarositeKFe33+(SO4)2(OH)6
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ Neotocite(Mn,Fe,Mg)SiO3 · H2O
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ AntleriteCu3(SO4)(OH)4
Cuβ“˜ AtacamiteCu2(OH)3Cl
Cuβ“˜ BorniteCu5FeS4
Cuβ“˜ BrochantiteCu4(SO4)(OH)6
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChalcanthiteCuSO4 · 5H2O
Cuβ“˜ ChalcociteCu2S
Cuβ“˜ Cuprite var. ChalcotrichiteCu2O
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ CovelliteCuS
Cuβ“˜ CupriteCu2O
Cuβ“˜ CopperCu
Cuβ“˜ DelafossiteCuFeO2
Cuβ“˜ MalachiteCu2(CO3)(OH)2
Cuβ“˜ TenoriteCuO
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
Cuβ“˜ TurquoiseCuAl6(PO4)4(OH)8 · 4H2O
ZnZinc
Znβ“˜ SphaleriteZnS
MoMolybdenum
Moβ“˜ MolybdeniteMoS2
SbAntimony
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
AuGold
Auβ“˜ GoldAu
PbLead
Pbβ“˜ GalenaPbS

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Link to USGS MRDS:10026888

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