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Fenian Gold Mine, Meekatharra Goldfield, Meekatharra, Meekatharra Shire, Western Australia, Australiai
Regional Level Types
Fenian Gold MineMine
Meekatharra GoldfieldOre Field
Meekatharra- not defined -
Meekatharra ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
26° 36' 37'' South , 118° 30' 16'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Meekatharra927 (2012)2.0km
Mindat Locality ID:
265442
Long-form identifier:
mindat:1:2:265442:6
GUID (UUID V4):
0


(Map- Google maps place the Meekatharra-Sandstone Road in the wrong position, and is actually east of the mine)

The Fenian gold mine (GML 477) is on the main Paddy's Flat line of lode about 1 kilometre east of Meekatharra. The Ingliston Extended mine borders it to the north, and the Marmont mine to the south. A modern abandoned open pit now marks the site developed in the 1990's.

The mine was initially pegged by F. Osborne and T Ryan in July 1903. It was initially worked at a loss. In October 1905 they purchased a battery from the Champion Mine Nannine. The mine was then developed by a small Perth syndicate of six men, with W.H. James the largest shareholder owning 380 of the 1200 shares in the company. The syndicate can be compared to Ebenezer Scrooge in its handling of the mine. A certain meanness pervades its actions from 1906 when they started development to 1923 when they sold the mine to the Ingliston Consols group.

These men must have started with significant funds already to be able to equip a fully functioning mine to the point of producing gold. Once running it produced 4000 pounds per month in dividends for the six shareholders, a small fortune in today's money. The syndicate was not on friendly terms, and in 1912 James took the other shareholders to court as they had approved a donation to a charity. James stated it was not the role of the syndicate to donate money to charitable causes, and didn't see why he should have to do this as the largest shareholder. He lost the action, and was forced to donate money to a hospital. The fuss was over 15 pounds.

The battery was gradually extended so by the end of the syndicates term it had a 20 head battery, cyanide and filter plant, and much other machinery, and was employing over one hundred men. The reef ranged from 11 to 18 feet wide.

Sam Carson (35) died from a fall of earth at the mine in 1907. In 1918 Swede Johann Anderson was killed when he fell into a shaft at the no. 3 level.

The mine was being operated in an unsafe manner placing the miner's health in danger. These short cuts were taking place to save money. When the Inspector of Mines would visit the practices stopped, only to return again after he had left. Facilities normally associated with mines of the time were not provided for employees. The wages were also poor in comparison, not helped by lavish dividends being paid to the shareholders. When the miners complained there was no facility to dry their wet clothes, the company burn't the clothes, leaving the miners nothing to wear to continue working. This last action sent the employees over the proverbial edge, and in 1916 there was a strike which lasted several months. Many left the district to seek employment on other mines elsewhere in Western Australia. The arbitration court eventually gave the men a pay rise and they returned to work.

In 1918, it is reported the mine has produced 384 105 pounds of dividends to its six shareholders. The last crushing was found in 1919, and it is thought the rich chutes the company was mining ran out. Based on a geologist's report that there was likely more gold at depth, the neighbouring Ingliston Consols took over the mine in 1923, and re-opened it in conjunction with its own mine.

Shears and cross shear veins carry valuable gold in this mine. The main ore channel in the mineralised shear zone strikes north north-east, dips east, with numerous milky white quartz veins. The ore body at Fenian is narrower than neighbouring mines, with a higher proportion of quartz, and a complex system of large cross veins.

Mines in the area are being filled in subsequent to this being written.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


13 valid minerals.

Rock Types Recorded

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

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Albite
Formula: Na(AlSi3O8)
Ankerite
Formula: Ca(Fe2+,Mg)(CO3)2
Antigorite
Formula: Mg3(Si2O5)(OH)4
Arsenopyrite
Formula: FeAsS
'Chlorite Group'
Chrysotile
Formula: Mg3(Si2O5)(OH)4
Kaolinite
Formula: Al2(Si2O5)(OH)4
Magnesite
Formula: MgCO3
Magnesite var. Mesitine Spar
Formula: (Mg,Fe)CO3
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Fuchsite
Formula: K(Al,Cr)3Si3O10(OH)2
Native Gold
Formula: Au
Pyrite
Formula: FeS2
Quartz
Formula: SiO2
Talc
Formula: Mg3Si4O10(OH)2
Zoisite
Formula: (CaCa)(AlAlAl)O[Si2O7][SiO4](OH)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Pyrite2.EB.05aFeS2
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Magnesite5.AB.05MgCO3
var. Mesitine Spar5.AB.05(Mg,Fe)CO3
Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
Group 9 - Silicates
Chrysotile9.00.Mg3(Si2O5)(OH)4
Zoisite9.BG.10(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Talc9.EC.05Mg3Si4O10(OH)2
Muscovite
var. Fuchsite
9.EC.15K(Al,Cr)3Si3O10(OH)2
9.EC.15KAl2(AlSi3O10)(OH)2
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Antigorite9.ED.15Mg3(Si2O5)(OH)4
Albite9.FA.35Na(AlSi3O8)
Unclassified
'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
H AntigoriteMg3(Si2O5)(OH)4
H ChrysotileMg3(Si2O5)(OH)4
H Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
H KaoliniteAl2(Si2O5)(OH)4
H MuscoviteKAl2(AlSi3O10)(OH)2
H TalcMg3Si4O10(OH)2
H Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
CCarbon
C AnkeriteCa(Fe2+,Mg)(CO3)2
C MagnesiteMgCO3
C Magnesite var. Mesitine Spar(Mg,Fe)CO3
OOxygen
O AlbiteNa(AlSi3O8)
O AnkeriteCa(Fe2+,Mg)(CO3)2
O AntigoriteMg3(Si2O5)(OH)4
O ChrysotileMg3(Si2O5)(OH)4
O Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
O KaoliniteAl2(Si2O5)(OH)4
O MagnesiteMgCO3
O MuscoviteKAl2(AlSi3O10)(OH)2
O QuartzSiO2
O TalcMg3Si4O10(OH)2
O Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
O Magnesite var. Mesitine Spar(Mg,Fe)CO3
NaSodium
Na AlbiteNa(AlSi3O8)
MgMagnesium
Mg AnkeriteCa(Fe2+,Mg)(CO3)2
Mg AntigoriteMg3(Si2O5)(OH)4
Mg ChrysotileMg3(Si2O5)(OH)4
Mg MagnesiteMgCO3
Mg TalcMg3Si4O10(OH)2
Mg Magnesite var. Mesitine Spar(Mg,Fe)CO3
AlAluminium
Al AlbiteNa(AlSi3O8)
Al Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Al KaoliniteAl2(Si2O5)(OH)4
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
SiSilicon
Si AlbiteNa(AlSi3O8)
Si AntigoriteMg3(Si2O5)(OH)4
Si ChrysotileMg3(Si2O5)(OH)4
Si Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
Si KaoliniteAl2(Si2O5)(OH)4
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si QuartzSiO2
Si TalcMg3Si4O10(OH)2
Si Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
SSulfur
S ArsenopyriteFeAsS
S PyriteFeS2
KPotassium
K Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
K MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca AnkeriteCa(Fe2+,Mg)(CO3)2
Ca Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
CrChromium
Cr Muscovite var. FuchsiteK(Al,Cr)3Si3O10(OH)2
FeIron
Fe AnkeriteCa(Fe2+,Mg)(CO3)2
Fe ArsenopyriteFeAsS
Fe PyriteFeS2
Fe Magnesite var. Mesitine Spar(Mg,Fe)CO3
AsArsenic
As ArsenopyriteFeAsS
AuGold
Au Native GoldAu

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

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