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Ragged Hills Mine, Braeside lead field, East Pilbara Shire, Western Australia, Australiai
Regional Level Types
Ragged Hills MineMine (Abandoned)
Braeside lead fieldMining Field (Abandoned)
East Pilbara ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
21° 17' 42'' South , 121° 8' 41'' East
Latitude & Longitude (decimal):
Type:
Mine (Abandoned) - last checked 2021
Köppen climate type:
Mindat Locality ID:
122734
Long-form identifier:
mindat:1:2:122734:8
GUID (UUID V4):
5460ab7d-6ca2-4db0-928f-e26af14d58d6


The Ragged Hills Mine is located 66 kilometres southeast of Warrawagine.

The Ragged Hills Mine can be located from the Telfer Mine road in the Gregory Ranges. Look for building foundations on the northern side of the road, next to a creek, and follow a track 200 metres in a northerly direction. Kim McDonald visited the mine in the late 1970's and in 2012. The processing plant and various mining equipment from when it was abandoned in 1959 still exists, slowly rusting away. It makes for a fascinating visit.

Massive galena is abundant on the dumps. It is hosted by two quartz filled faults, oriented in a north-west to south-east direction, along the top of the ridge for 30 metres. After mining, this formed a 46 metre deep chasm along the top of the hill. A short tunnel extends from the processing plant through the side of the hill to the chasm.

This is the largest of the deposits in the Braeside lead field. Two quartz-filled faults striking 340 degrees and dipping 80 degrees east (the regional trend of mineralized veins) follow a 30 metre ridge in sheared basalt, tuff and carbonate rocks of the Fortescue Group (Kylena Basalt). The volcanic rocks also strike north-northwest but dip at shallow angles to the west-southwest. Lead occurs over 300 metres, in a lode up to 4.2 metres wide in a cymoid loop split on the western fault. The mineralization forms massive lenses or disseminations in quartz and quartz-filled breccia and is mainly galena with small amounts of sphalerite, chalcopyrite, bornite and pyrite. Cerussite, anglesite and malachite are present in the oxidized zone.

The deposit was worked over 150 metres along strike and to 46 metres depth between 1925 and 1928, and from 1950 to 1959, for a total production of 2927.2 tonnes of lead, 24.4 tonnes of zinc and 874 kilograms of silver.

Galena, chalcocite, covellite, cerussite, malachite, rosasite, smithsonite, pyromorphite, hemimorphite, chrysocolla, kaolinite, quartz, goethite, hematite, coronadite, manganese oxides, plattnerite, anglesite, jarosite, plumbojarosite, sphalerite and opal have been identified from here.

The Simpson Mineral Collection of the Western Australian Museum contains specimens MDC 981, 1046, 1097, 1697, 4303 and 4677 from this location.

Details for this location are also taken from its entry (site code S0018172) in the Western Australian Department of Mines, Industry Regulation and Safety's online database (MINEDEX) of mines, mineral deposits and prospects.


Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


27 valid minerals.

Detailed Mineral List:

Anglesite
Formula: PbSO4
Bornite
Formula: Cu5FeS4
Cerussite
Formula: PbCO3
Chalcocite
Formula: Cu2S
Chalcopyrite
Formula: CuFeS2
'Chlorite Group'
Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Coronadite
Formula: Pb(Mn4+6Mn3+2)O16
Covellite
Formula: CuS
Descloizite
Formula: PbZn(VO4)(OH)
Galena
Formula: PbS
Goethite
Formula: α-Fe3+O(OH)
Hematite
Formula: Fe2O3
Hemimorphite
Formula: Zn4Si2O7(OH)2 · H2O
Hydrozincite
Formula: Zn5(CO3)2(OH)6
Jarosite
Formula: KFe3+3(SO4)2(OH)6
Kaolinite
Formula: Al2(Si2O5)(OH)4
'Limonite'
Malachite
Formula: Cu2(CO3)(OH)2
'Manganese Oxides'
Opal
Formula: SiO2 · nH2O
Plattnerite
Formula: PbO2
Plumbojarosite
Formula: Pb0.5Fe3+3(SO4)2(OH)6
Pyrite
Formula: FeS2
Pyromorphite
Formula: Pb5(PO4)3Cl
Quartz
Formula: SiO2
Rosasite
Formula: (Cu,Zn)2(CO3)(OH)2
Smithsonite
Formula: ZnCO3
Sphalerite
Formula: ZnS
Vanadinite
Formula: Pb5(VO4)3Cl

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcocite2.BA.05Cu2S
Bornite2.BA.15Cu5FeS4
Covellite2.CA.05aCuS
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Goethite4.00.α-Fe3+O(OH)
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Opal4.DA.10SiO2 · nH2O
Plattnerite4.DB.05PbO2
Coronadite4.DK.05aPb(Mn4+6Mn3+2)O16
Group 5 - Nitrates and Carbonates
Smithsonite5.AB.05ZnCO3
Cerussite5.AB.15PbCO3
Rosasite5.BA.10(Cu,Zn)2(CO3)(OH)2
Malachite5.BA.10Cu2(CO3)(OH)2
Hydrozincite5.BA.15Zn5(CO3)2(OH)6
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Anglesite7.AD.35PbSO4
Plumbojarosite7.BC.10Pb0.5Fe3+3(SO4)2(OH)6
Jarosite7.BC.10KFe3+3(SO4)2(OH)6
Group 8 - Phosphates, Arsenates and Vanadates
Descloizite8.BH.40PbZn(VO4)(OH)
Pyromorphite8.BN.05Pb5(PO4)3Cl
Vanadinite8.BN.05Pb5(VO4)3Cl
Group 9 - Silicates
Hemimorphite9.BD.10Zn4Si2O7(OH)2 · H2O
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Unclassified
'Limonite'-
'Chlorite Group'-
'Manganese Oxides'-

List of minerals for each chemical element

HHydrogen
H ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
H DescloizitePbZn(VO4)(OH)
H Goethiteα-Fe3+O(OH)
H HemimorphiteZn4Si2O7(OH)2 · H2O
H HydrozinciteZn5(CO3)2(OH)6
H JarositeKFe33+(SO4)2(OH)6
H KaoliniteAl2(Si2O5)(OH)4
H MalachiteCu2(CO3)(OH)2
H OpalSiO2 · nH2O
H PlumbojarositePb0.5Fe33+(SO4)2(OH)6
H Rosasite(Cu,Zn)2(CO3)(OH)2
CCarbon
C CerussitePbCO3
C HydrozinciteZn5(CO3)2(OH)6
C MalachiteCu2(CO3)(OH)2
C Rosasite(Cu,Zn)2(CO3)(OH)2
C SmithsoniteZnCO3
OOxygen
O AnglesitePbSO4
O CerussitePbCO3
O ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
O CoronaditePb(Mn64+Mn23+)O16
O DescloizitePbZn(VO4)(OH)
O Goethiteα-Fe3+O(OH)
O HematiteFe2O3
O HemimorphiteZn4Si2O7(OH)2 · H2O
O HydrozinciteZn5(CO3)2(OH)6
O JarositeKFe33+(SO4)2(OH)6
O KaoliniteAl2(Si2O5)(OH)4
O MalachiteCu2(CO3)(OH)2
O OpalSiO2 · nH2O
O PlattneritePbO2
O PlumbojarositePb0.5Fe33+(SO4)2(OH)6
O PyromorphitePb5(PO4)3Cl
O QuartzSiO2
O Rosasite(Cu,Zn)2(CO3)(OH)2
O SmithsoniteZnCO3
O VanadinitePb5(VO4)3Cl
AlAluminium
Al ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Al KaoliniteAl2(Si2O5)(OH)4
SiSilicon
Si ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Si HemimorphiteZn4Si2O7(OH)2 · H2O
Si KaoliniteAl2(Si2O5)(OH)4
Si OpalSiO2 · nH2O
Si QuartzSiO2
PPhosphorus
P PyromorphitePb5(PO4)3Cl
SSulfur
S AnglesitePbSO4
S BorniteCu5FeS4
S ChalcopyriteCuFeS2
S ChalcociteCu2S
S CovelliteCuS
S GalenaPbS
S JarositeKFe33+(SO4)2(OH)6
S PlumbojarositePb0.5Fe33+(SO4)2(OH)6
S PyriteFeS2
S SphaleriteZnS
ClChlorine
Cl PyromorphitePb5(PO4)3Cl
Cl VanadinitePb5(VO4)3Cl
KPotassium
K JarositeKFe33+(SO4)2(OH)6
VVanadium
V DescloizitePbZn(VO4)(OH)
V VanadinitePb5(VO4)3Cl
MnManganese
Mn CoronaditePb(Mn64+Mn23+)O16
FeIron
Fe BorniteCu5FeS4
Fe ChalcopyriteCuFeS2
Fe Goethiteα-Fe3+O(OH)
Fe HematiteFe2O3
Fe JarositeKFe33+(SO4)2(OH)6
Fe PlumbojarositePb0.5Fe33+(SO4)2(OH)6
Fe PyriteFeS2
CuCopper
Cu BorniteCu5FeS4
Cu ChalcopyriteCuFeS2
Cu ChalcociteCu2S
Cu ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cu CovelliteCuS
Cu MalachiteCu2(CO3)(OH)2
Cu Rosasite(Cu,Zn)2(CO3)(OH)2
ZnZinc
Zn DescloizitePbZn(VO4)(OH)
Zn HemimorphiteZn4Si2O7(OH)2 · H2O
Zn HydrozinciteZn5(CO3)2(OH)6
Zn Rosasite(Cu,Zn)2(CO3)(OH)2
Zn SmithsoniteZnCO3
Zn SphaleriteZnS
PbLead
Pb AnglesitePbSO4
Pb CerussitePbCO3
Pb CoronaditePb(Mn64+Mn23+)O16
Pb DescloizitePbZn(VO4)(OH)
Pb GalenaPbS
Pb PlattneritePbO2
Pb PlumbojarositePb0.5Fe33+(SO4)2(OH)6
Pb PyromorphitePb5(PO4)3Cl
Pb VanadinitePb5(VO4)3Cl

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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