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Copper Claim (Anesbury mine), Eurelia, South Flinders Ranges, Flinders Ranges, South Australia, Australiai
Regional Level Types
Copper Claim (Anesbury mine)Claim
Eurelia- not defined -
South Flinders Ranges- not defined -
Flinders RangesMining Region
South AustraliaState
AustraliaCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
32° 31' 32'' South , 138° 29' 9'' East
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Carrieton130 (2013)11.2km
Orroroo632 (2013)26.1km
Pekina171 (2012)34.7km
Booleroo486 (2018)34.8km
Wilmington628 (2013)38.8km
Mindat Locality ID:
203795
Long-form identifier:
mindat:1:2:203795:3
GUID (UUID V4):
4ddc6839-8063-4787-828a-3690d51e3319


Prospecting originally commenced here in 1943, when claims were taken up on this section (hundred of Eurelia). Accompanied by intermittent prospecting until 1948, at which time H.L.Anesbury took up claim M.C. 1323, holding it for a year. During this time 153 pounds of copper was produced from one ton of ore (the only recorded production from this locality to date - 2016). Since that time, three other claims have been held on this locality prior to the commencement of exploration by the Utah Development Co. Ltd .

Situated amongst stratiform copper mineralisation an area of 2.5 by 1 km was explored by Utah (beginning in 1969), with drilling beginning 1971. Occurring near the core of a south-west plunging anticline within the Burra Group. The host rocks can be classified as carbonaceous and pyritic siltstone, dolomite, and arenite, with magnesite conglomerate, and interbedded chert. Mineralisation consisted primarily of chalcopyrite and pyrite in quartz and calcite veins disseminated within host rocks. Secondary malachite, chalcocite, native copper and cupriferous chlorite, were also recorded.


Located approximately 260 km north of Adelaide; and 7.5 km east of Eurelia.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


28 valid minerals.

Detailed Mineral List:

β“˜ Albite
Formula: Na(AlSi3O8)
Description: "The felspars consist of a mixture of microcline, oligoclase and orthoclase. all crystals tend to be marginally corroded and argillised, which may be due to hydrolytic effects associated with metasomatic introduction of hematite" -12- pg143, R0B05.P

"Felspars are principally potassic varieties, microcline and turbid argillised orthoclases, but with a minor proportion of plagioclase, oglioclase to andesine in composition." -14- pg 183, ED02/0618.3/00.2P

Notes taken from Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Albite var. Andesine
Formula: (Na,Ca)[Al(Si,Al)Si2O8]
Description: "The felspars consist of a mixture of microcline, oligoclase and orthoclase. all crystals tend to be marginally corroded and argillised, which may be due to hydrolytic effects associated with metasomatic introduction of hematite" -12- pg143, R0B05.P

"Felspars are principally potassic varieties, microcline and turbid argillised orthoclases, but with a minor proportion of plagioclase, oglioclase to andesine in composition." -14- pg 183, ED02/0618.3/00.2P

Notes taken from Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Albite var. Oligoclase
Formula: (Na,Ca)[Al(Si,Al)Si2O8]
Description: "The felspars consist of a mixture of microcline, oligoclase and orthoclase. all crystals tend to be marginally corroded and argillised, which may be due to hydrolytic effects associated with metasomatic introduction of hematite" -12- pg143, R0B05.P

"Felspars are principally potassic varieties, microcline and turbid argillised orthoclases, but with a minor proportion of plagioclase, oglioclase to andesine in composition." -14- pg 183, ED02/0618.3/00.2P

Notes taken from Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
β“˜ Azurite
Formula: Cu3(CO3)2(OH)2
β“˜ Bornite
Formula: Cu5FeS4
β“˜ Calcite
Formula: CaCO3
β“˜ Chalcocite
Formula: Cu2S
β“˜ Chalcopyrite
Formula: CuFeS2
β“˜ 'Chlorite Group'
β“˜ Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
β“˜ Copper
Formula: Cu
β“˜ Cuprite
Formula: Cu2O
β“˜ Dolomite
Formula: CaMg(CO3)2
β“˜ 'Feldspar Group'
Description: "The felspars consist of a mixture of microcline, oligoclase and orthoclase. all crystals tend to be marginally corroded and argillised, which may be due to hydrolytic effects associated with metasomatic introduction of hematite" -12- pg143, R0B05.P

"Felspars are principally potassic varieties, microcline and turbid argillised orthoclases, but with a minor proportion of plagioclase, oglioclase to andesine in composition." -14- pg 183, ED02/0618.3/00.2P

Notes taken from Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Goethite
Formula: Ξ±-Fe3+O(OH)
β“˜ Graphite
Formula: C
β“˜ Hematite
Formula: Fe2O3
β“˜ Jarosite
Formula: KFe3+3(SO4)2(OH)6
β“˜ 'Limonite'
Description: Noted as pseudomorphs after pyrite. - Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Mackinawite
Formula: FeS
β“˜ Magnesite
Formula: MgCO3
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
β“˜ Malachite
Formula: Cu2(CO3)(OH)2
β“˜ Marcasite
Formula: FeS2
β“˜ Microcline
Formula: K(AlSi3O8)
Description: "The felspars consist of a mixture of microcline, oligoclase and orthoclase. all crystals tend to be marginally corroded and argillised, which may be due to hydrolytic effects associated with metasomatic introduction of hematite" -12- pg143, R0B05.P

"Felspars are principally potassic varieties, microcline and turbid argillised orthoclases, but with a minor proportion of plagioclase, oglioclase to andesine in composition." -14- pg 183, ED02/0618.3/00.2P

Notes taken from Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Orthoclase
Formula: K(AlSi3O8)
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Listed as 'plagioclase' by Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)

"The felspars consist of a mixture of microcline, oligoclase and orthoclase. all crystals tend to be marginally corroded and argillised, which may be due to hydrolytic effects associated with metasomatic introduction of hematite" -12- pg143, R0B05.P

"Felspars are principally potassic varieties, microcline and turbid argillised orthoclases, but with a minor proportion of plagioclase, oglioclase to andesine in composition." -14- pg 183, ED02/0618.3/00.2P

Notes taken from Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Pyrite
Formula: FeS2
β“˜ Pyrrhotite
Formula: Fe1-xS
β“˜ Quartz
Formula: SiO2
β“˜ Titanite
Formula: CaTi(SiO4)O
Description: Listed as 'sphene' by Rowlands, N.J., Stuart, N.F., & Edwards, P. (1972)
β“˜ Topaz
Formula: Al2(SiO4)(F,OH)2
β“˜ 'Tourmaline'
Formula: AD3G6 (T6O18)(BO3)3X3Z
β“˜ Zircon
Formula: Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Copper1.AA.05Cu
β“˜Graphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
β“˜Chalcocite2.BA.05Cu2S
β“˜Bornite2.BA.15Cu5FeS4
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Pyrrhotite2.CC.10Fe1-xS
β“˜Mackinawite2.CC.25FeS
β“˜Pyrite2.EB.05aFeS2
β“˜Marcasite2.EB.10aFeS2
Group 4 - Oxides and Hydroxides
β“˜Goethite4.00.Ξ±-Fe3+O(OH)
β“˜Cuprite4.AA.10Cu2O
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Hematite4.CB.05Fe2O3
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Magnesite5.AB.05MgCO3
β“˜Calcite5.AB.05CaCO3
β“˜Dolomite5.AB.10CaMg(CO3)2
β“˜Azurite5.BA.05Cu3(CO3)2(OH)2
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Jarosite7.BC.10KFe3+3(SO4)2(OH)6
Group 9 - Silicates
β“˜Zircon9.AD.30Zr(SiO4)
β“˜Topaz9.AF.35Al2(SiO4)(F,OH)2
β“˜Titanite9.AG.15CaTi(SiO4)O
β“˜Muscovite
var. Sericite
9.EC.15KAl2(AlSi3O10)(OH)2
β“˜9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1
β“˜Microcline9.FA.30K(AlSi3O8)
β“˜Orthoclase9.FA.30K(AlSi3O8)
β“˜Albite9.FA.35Na(AlSi3O8)
β“˜var. Oligoclase9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
β“˜var. Andesine9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
Unclassified
β“˜'Limonite'-
β“˜'Tourmaline'-AD3G6 (T6O18)(BO3)3X3Z
β“˜'Feldspar Group'-
β“˜'Chlorite Group'-
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'Apatite'-Ca5(PO4)3(Cl/F/OH)

List of minerals for each chemical element

HHydrogen
Hβ“˜ AzuriteCu3(CO3)2(OH)2
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ GoethiteΞ±-Fe3+O(OH)
Hβ“˜ JarositeKFe33+(SO4)2(OH)6
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ TopazAl2(SiO4)(F,OH)2
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Hβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
BBoron
Bβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
CCarbon
Cβ“˜ AzuriteCu3(CO3)2(OH)2
Cβ“˜ CalciteCaCO3
Cβ“˜ DolomiteCaMg(CO3)2
Cβ“˜ GraphiteC
Cβ“˜ MagnesiteMgCO3
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ Albite var. Andesine(Na,Ca)[Al(Si,Al)Si2O8]
Oβ“˜ AzuriteCu3(CO3)2(OH)2
Oβ“˜ CalciteCaCO3
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ CupriteCu2O
Oβ“˜ DolomiteCaMg(CO3)2
Oβ“˜ GoethiteΞ±-Fe3+O(OH)
Oβ“˜ HematiteFe2O3
Oβ“˜ JarositeKFe33+(SO4)2(OH)6
Oβ“˜ MagnesiteMgCO3
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ MicroclineK(AlSi3O8)
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Oβ“˜ OrthoclaseK(AlSi3O8)
Oβ“˜ QuartzSiO2
Oβ“˜ TitaniteCaTi(SiO4)O
Oβ“˜ TopazAl2(SiO4)(F,OH)2
Oβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
Oβ“˜ ZirconZr(SiO4)
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
Fβ“˜ TopazAl2(SiO4)(F,OH)2
Fβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ Albite var. Andesine(Na,Ca)[Al(Si,Al)Si2O8]
Naβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ DolomiteCaMg(CO3)2
Mgβ“˜ MagnesiteMgCO3
AlAluminium
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ Albite var. Andesine(Na,Ca)[Al(Si,Al)Si2O8]
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Alβ“˜ MicroclineK(AlSi3O8)
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Alβ“˜ OrthoclaseK(AlSi3O8)
Alβ“˜ TopazAl2(SiO4)(F,OH)2
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ Albite var. Andesine(Na,Ca)[Al(Si,Al)Si2O8]
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ MicroclineK(AlSi3O8)
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Siβ“˜ OrthoclaseK(AlSi3O8)
Siβ“˜ QuartzSiO2
Siβ“˜ TitaniteCaTi(SiO4)O
Siβ“˜ TopazAl2(SiO4)(F,OH)2
Siβ“˜ ZirconZr(SiO4)
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
Sβ“˜ BorniteCu5FeS4
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ ChalcociteCu2S
Sβ“˜ JarositeKFe33+(SO4)2(OH)6
Sβ“˜ MackinawiteFeS
Sβ“˜ MarcasiteFeS2
Sβ“˜ PyriteFeS2
Sβ“˜ PyrrhotiteFe1-xS
ClChlorine
Clβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
Kβ“˜ JarositeKFe33+(SO4)2(OH)6
Kβ“˜ MicroclineK(AlSi3O8)
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ OrthoclaseK(AlSi3O8)
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ Albite var. Andesine(Na,Ca)[Al(Si,Al)Si2O8]
Caβ“˜ CalciteCaCO3
Caβ“˜ DolomiteCaMg(CO3)2
Caβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Caβ“˜ TitaniteCaTi(SiO4)O
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Caβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
Tiβ“˜ TitaniteCaTi(SiO4)O
FeIron
Feβ“˜ BorniteCu5FeS4
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ GoethiteΞ±-Fe3+O(OH)
Feβ“˜ HematiteFe2O3
Feβ“˜ JarositeKFe33+(SO4)2(OH)6
Feβ“˜ MackinawiteFeS
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ MarcasiteFeS2
Feβ“˜ PyriteFeS2
Feβ“˜ PyrrhotiteFe1-xS
CuCopper
Cuβ“˜ AzuriteCu3(CO3)2(OH)2
Cuβ“˜ BorniteCu5FeS4
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChalcociteCu2S
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ CupriteCu2O
Cuβ“˜ CopperCu
Cuβ“˜ MalachiteCu2(CO3)(OH)2
ZrZirconium
Zrβ“˜ ZirconZr(SiO4)

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