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Warrawoona Gold Project, Marble Bar, East Pilbara Shire, Western Australia, Australiai
Regional Level Types
Warrawoona Gold ProjectGroup of Mines
Marble Bar- not defined -
East Pilbara ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
21° 17' 9'' South , 119° 49' 40'' East
Latitude & Longitude (decimal):
Type:
Group of Mines
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Marble Bar612 (2012)15.5km
Mindat Locality ID:
247455
Long-form identifier:
mindat:1:2:247455:0
GUID (UUID V4):
60ebc20a-4512-411a-8c35-51becefb4e2f


From Calidus Resources Ltd website, in 2020 "The Warrawoona Gold Project is situated in the East Pilbara district of the Pilbara Goldfield of Western Australia, approximately 150km south east of Port Hedland and approximately 25km south east of the town of Marble Bar.

Historically fragmented ownership has held back development of the area. Calidus now controls the entire Warrawoona Greenstone Belt with a total of 780km2 under its control. Since listing in mid-2017 with a resource of 411kozs, the Company has undertaken a systematic modern approach to exploration and tripled the resource base to its current 1.5 million ounces."

In 2020, the Company controlled the entire Warrawoona greenstone belt and held over 200 historic workings on these tenements.

The Salgash field is a long forgotten goldfield. The general impression is initial gold discoveries on and near the surface were incredibly rich, but didn't extend at depth to any great extent. It is 20 kilometres south south-east of Marble Bar.

Charles Kopeke (sometimes spelt Kopecke) is credited for discovering the gold reef in 1897 which ran for miles over the hills. He pegged a claim called Reward. Early reports described the whole region from Marble Bar to Nullagine as The Salgash Belt. It was also a town, although a writer in 1899 states it had two hotels, a bush telegraph office and little else, although one hundred men were working the surrounding goldfield at this time. In 1898, the inhabitants of Salgash insisted the town's name be changed to the indigenous Warrawoona.

The next lease pegged by W.J. Corboy and Pontt, called Klondyke at 6 acres.
They drove an access tunnel into the hill, lined with free coarse gold in quartz. Virtually the entire town of Marble Bar left the next day for the goldfield. Initial gold discoveries along the reef were spectacular, outcropping for about 6 kilometres, 60 to 100 tonnes of gold on the surface. Pilbara Inspector of Mines, E. Davenport Cleland, made a detailed report on the goldfield in 1909, but the goldfield was already in decline.

All the mines at this time were operated by single prospectors or small local syndicates. Bow Bells was the first mine visited which had a ten head battery but no mining was taking place. The Gauntlet Mine at 12 acres
had a small plant but also no mining on a shaft 42 metres down. It was on a large reef with poor gold grades. The mine described as being in a bad condition. It was originally pegged in 1898 by Mackenzie and Corbett

The Gift Mine was south-east of Bow Bells, owned by Richards and Bradley, who had abandoned the mine due to the small vein it was on and the inflow of water. South-east of Gift was the Golden Gauntlet Mine with a shaft 15 metres deep, on a reef 60-80 cms wide, and a shoot 3 metres long.

The Klondyke Boulder Mine was operating on five reefs but was struggling to stay above water (literally) which was flooding the underground workings. A newish main shaft had been sunk through soft schist between the south and main (or blue) reefs. It employed twelve men with a five head battery. In 1909 it was worked by H. Cooper, M.L. Cooke, and Frank Atkinson. It is also stated in 1910 the liquidators had taken over the mine on behalf of the British Exploration Company, which had gone bankrupt several years before. Around 1909 it applied for government assistance to develop the mine, and good gold was found in 1912, but nothing was noted after this.

The Klondyke Queen Mine was owned by Royer and Aitkins, on a very small reef, dipping at a high angle west. They had constructed a tunnel 131 metres into the hill following it. In 1914 it closed. Next was an un-named shaft Davenport Cleland found contained quartz coated with a thin film of gold.

Continuing south-east, the old St George workings, Cuban, Britannia Mines were all abandoned. St George was near the crest of the hill to the north of the bar. Alluvial gullies below this had been worked with some success. Cuban and Britannia were on the south side of the bar on the Kopeke leader. Beyond this was Daly, Frederick and Vereo lease, and adjacent to the south J. O'Connors shaft. At the foot of the range on the south side of the bar was a new lease called Koombana on a well defined reef, 213-243 metres along the surface.

No reference to mining was found after 1914 until some small scale mining occurred in the 1930's by pairs or lone prospectors, then nothing. Other mines in the area are Cairns and Franklin Mines 10 kms north; Apex and Phoenix 5 kms west at the northern end of the Salgash field, Euro and Coppenhagen near the track 5 kms west from the middle section of Salgash and Princept two kms west; Wheel of Fortune and Charlie Mines west at the southern end of the field.

The area has produced officially 0.94 tonnes of gold. It has a JORC resource of 9.10 tonnes of gold. The deposits are associated with the Klondyke Shear Zone, which cuts a synclinal structure between the Mount Edgar and Corunna Downs granitic complexes. Most of the deposits are within 50 metres and parallel to the shear zone, in mafic and ultramafic rocks of the Apex Basalt.

The largest deposits are within sericitic schist to the south of a narrow (under 2 metre) sub vertical mylonitized chert known as the Kopekes Leader. There is an early alteration phase of carbonate-chlorite-talc-quartz, and later ore stage of sericite-pyrite-fuchsite. Gold mineralisation is within 10-30 mm wide boundinaged veins within sericite-pyrite selvages. Other minerals include chalcopyrite with minor sphalerite and galena. The veins shows as chocolate tablet boundinage with horizontal and vertical extension.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

22 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Rock list contains entries from the region specified including sub-localities

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

β“˜ Actinolite
Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
β“˜ Albite
Formula: Na(AlSi3O8)
β“˜ Ankerite
Formula: Ca(Fe2+,Mg)(CO3)2
β“˜ Azurite
Formula: Cu3(CO3)2(OH)2
β“˜ Calcite
Formula: CaCO3
β“˜ Chalcopyrite
Formula: CuFeS2
β“˜ 'Chlorite Group'
Localities: Reported from at least 7 localities in this region.
β“˜ Chromite
Formula: Fe2+Cr3+2O4
β“˜ Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
β“˜ Cuprite
Formula: Cu2O
β“˜ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜ Galena
Formula: PbS
β“˜ Gold
Formula: Au
Localities: Reported from at least 38 localities in this region.
β“˜ Hematite
Formula: Fe2O3
β“˜ Ilmenite
Formula: Fe2+TiO3
β“˜ 'Leucoxene'
β“˜ 'Limonite'
β“˜ Malachite
Formula: Cu2(CO3)(OH)2
Localities: Reported from at least 6 localities in this region.
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Muscovite var. Fuchsite
Formula: K(Al,Cr)3Si3O10(OH)2
β“˜ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
β“˜ Pyrite
Formula: FeS2
Localities: Reported from at least 9 localities in this region.
β“˜ Quartz
Formula: SiO2
Localities: Reported from at least 27 localities in this region.
β“˜ Quartz var. Chalcedony
Formula: SiO2
β“˜ 'Serpentine Subgroup'
Formula: D3[Si2O5](OH)4
β“˜ Siderite
Formula: FeCO3
β“˜ Sphalerite
Formula: ZnS
β“˜ Talc
Formula: Mg3Si4O10(OH)2
β“˜ 'Wad'
β“˜ Zoisite
Formula: (CaCa)(AlAlAl)O[Si2O7][SiO4](OH)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
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“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Ilmenite4.CB.05Fe2+TiO3
β“˜Hematite4.CB.05Fe2O3
β“˜Quartz
var. Chalcedony
4.DA.05SiO2
β“˜4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
β“˜Siderite5.AB.05FeCO3
β“˜Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
β“˜Azurite5.BA.05Cu3(CO3)2(OH)2
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 9 - Silicates
β“˜Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜Zoisite9.BG.10(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
β“˜Actinolite9.DE.10β—»Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
β“˜Talc9.EC.05Mg3Si4O10(OH)2
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Fuchsite9.EC.15K(Al,Cr)3Si3O10(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1
β“˜Albite9.FA.35Na(AlSi3O8)
Unclassified
β“˜'Limonite'-
β“˜'Wad'-
β“˜'Chlorite Group'-
β“˜'Leucoxene'-
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'Serpentine Subgroup'-D3[Si2O5](OH)4

List of minerals for each chemical element

HHydrogen
Hβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Hβ“˜ AzuriteCu3(CO3)2(OH)2
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hβ“˜ Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ TalcMg3Si4O10(OH)2
Hβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Hβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
CCarbon
Cβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Cβ“˜ AzuriteCu3(CO3)2(OH)2
Cβ“˜ CalciteCaCO3
Cβ“˜ MalachiteCu2(CO3)(OH)2
Cβ“˜ SideriteFeCO3
OOxygen
Oβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Oβ“˜ AzuriteCu3(CO3)2(OH)2
Oβ“˜ CalciteCaCO3
Oβ“˜ Quartz var. ChalcedonySiO2
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ CupriteCu2O
Oβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oβ“˜ Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Oβ“˜ HematiteFe2O3
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ QuartzSiO2
Oβ“˜ SideriteFeCO3
Oβ“˜ TalcMg3Si4O10(OH)2
Oβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
NaSodium
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Mgβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Mgβ“˜ TalcMg3Si4O10(OH)2
AlAluminium
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Alβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alβ“˜ Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ Quartz var. ChalcedonySiO2
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siβ“˜ Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ QuartzSiO2
Siβ“˜ TalcMg3Si4O10(OH)2
Siβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ GalenaPbS
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
KPotassium
Kβ“˜ Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Caβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Caβ“˜ CalciteCaCO3
Caβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Caβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiβ“˜ IlmeniteFe2+TiO3
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
Crβ“˜ Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
FeIron
Feβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Feβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feβ“˜ HematiteFe2O3
Feβ“˜ IlmeniteFe2+TiO3
Feβ“˜ PyriteFeS2
Feβ“˜ SideriteFeCO3
CuCopper
Cuβ“˜ AzuriteCu3(CO3)2(OH)2
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ CupriteCu2O
Cuβ“˜ MalachiteCu2(CO3)(OH)2
ZnZinc
Znβ“˜ SphaleriteZnS
AuGold
Auβ“˜ GoldAu
PbLead
Pbβ“˜ GalenaPbS

Localities in this Region

Other Regions, Features and Areas containing this locality

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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.

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