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Lisheen mine, Moyne, Tipperary County, Munster, Irelandi
| Regional Level Types | |
|---|---|
| Lisheen mine | Mine (Active) |
| Moyne | - not defined - |
| Tipperary County | County |
| Munster | Province |
| Ireland | Country |
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Latitude & Longitude (WGS84):
52° 44' 52'' North , 7° 40' 23'' West
Latitude & Longitude (decimal):
Type:
Mine (Active) - last checked 2019
Age:
358.9 ± 0.4 to 298.9 ± 0.15 Ma
Geologic Time:
Reference for age:
Bergakademie Freiberg, special display, 2019.
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Templetuohy | 323 (2013) | 5.4km |
| Urlingford | 973 (2013) | 6.8km |
| Johnstown | 472 (2013) | 8.0km |
| Twomileborris | 548 (2013) | 9.0km |
| Gortnahoe | 304 (2013) | 9.3km |
Stratabound, carbonate-hosted Zn-Pb deposit.
The orebody was found in 1990 using soil geochemistry, and mining commenced in 1997. Delays caused by higher than expected water ingress meant that the first ore was not produced until September 1999. The deposit was initially worked by an Anglo American-Ivernia West joint venture, until Anglo bought out Ivernia's share in 2003. They then sold out to Vedanta in 2010. The mine produced 5,000 tonnes of ore every working day, and closed at the end of 2015 following exhaustion of the economic reserves, having produced 22.3 million tonnes grading 11.7 % Zn and 2.0 % Pb. A further 4.4 million tonnes, grading 14.5 % Zn and 2.6 % Pb remains in the ground, for various reasons (sub-economic, inaccessible or unsuitable for mining for geotechnical reasons). The main ores consisted of galena, sphalerite and pyrite found as compact fine-grained material.
Lisheen orebodies are usually stratiform, varying in thickness from 1 m to 30 m and "room and pillar" mining was the predominant method used for extraction, though "drift and fill" and "long hole stoping" were also employed according to conditions. The Main Zone, which had distinct northern and southern halves, lay at the west end of the mineralized area. A few hundred meters east of this was the substantial Derryville Zone and two smaller ones further east again (Bog Zone West & Bog Zone East). The discovery, in 2005, of a satellite orebody (Island Pod) over half a kilometer to the NNW of the northern tip of Derryville Zone, added another two years to the mine's life. The orebodies were divided up into north, south, east zones etc., these in turn were divided into panels.
Thousands of tonnes of massive nickel arsenide ore (gersdorffite and nickeline) were found in the Killoran fault zone, in the southern part of the Main Zone. For a while a stockpile of this lay underground, soon becoming coated with soft green annabergite. Fragments of limestone mixed in with this acquired encrustations of pharmacolite, all post-mining and forming within a matter of months. Unfortunately, the high arsenic content of this ore deterred smelting companies, and no buyer could be found. Thousands of tonnes of rich copper ore (chalcocite, bornite, tennantite) also occurring along fault zones likewise failed to find a buyer owing to an inability to guarantee a consistent grade, despite its high (sometimes ca. 1 %) silver content.
The orebodies were compact and vugs, even of calcite, scarce. However, a few dozen small specimens of bright yellow sphalerite crystals were recovered from one small area (Panel 18) in the Main Zone (North). Most Lisheen sphalerite was dark treacle brown, and good crystallised specimens are very rare.
The Lisheen deposit is situated in the southern Irish Zn-Pb orefield, was the second largest mined Zn-Pb deposit in Ireland, with the resource (23 Mt @ 13.3 % Zn and 2.3 % Pb) mined from 1999 until 2015. At Lisheen, mineralisation is predominantly hosted by the Waulsortian Limestone Formation, which has been the focus of most published research. However, while minor, significant resources are located in the LOM of the underlying Ballysteen Formation, with notable Cu-Ni associations. The deposit contained six stratabound orebodies: Main Zone, Derryville, Bog East, Bog Central, Bog West and the Island Pod. Additional subeconomic mineralisation has been discovered at Barnalisheen to the northwest, and at Templetouhy and Bawnmore further east.
The orebody was found in 1990 using soil geochemistry, and mining commenced in 1997. Delays caused by higher than expected water ingress meant that the first ore was not produced until September 1999. The deposit was initially worked by an Anglo American-Ivernia West joint venture, until Anglo bought out Ivernia's share in 2003. They then sold out to Vedanta in 2010. The mine produced 5,000 tonnes of ore every working day, and closed at the end of 2015 following exhaustion of the economic reserves, having produced 22.3 million tonnes grading 11.7 % Zn and 2.0 % Pb. A further 4.4 million tonnes, grading 14.5 % Zn and 2.6 % Pb remains in the ground, for various reasons (sub-economic, inaccessible or unsuitable for mining for geotechnical reasons). The main ores consisted of galena, sphalerite and pyrite found as compact fine-grained material.
Lisheen orebodies are usually stratiform, varying in thickness from 1 m to 30 m and "room and pillar" mining was the predominant method used for extraction, though "drift and fill" and "long hole stoping" were also employed according to conditions. The Main Zone, which had distinct northern and southern halves, lay at the west end of the mineralized area. A few hundred meters east of this was the substantial Derryville Zone and two smaller ones further east again (Bog Zone West & Bog Zone East). The discovery, in 2005, of a satellite orebody (Island Pod) over half a kilometer to the NNW of the northern tip of Derryville Zone, added another two years to the mine's life. The orebodies were divided up into north, south, east zones etc., these in turn were divided into panels.
Thousands of tonnes of massive nickel arsenide ore (gersdorffite and nickeline) were found in the Killoran fault zone, in the southern part of the Main Zone. For a while a stockpile of this lay underground, soon becoming coated with soft green annabergite. Fragments of limestone mixed in with this acquired encrustations of pharmacolite, all post-mining and forming within a matter of months. Unfortunately, the high arsenic content of this ore deterred smelting companies, and no buyer could be found. Thousands of tonnes of rich copper ore (chalcocite, bornite, tennantite) also occurring along fault zones likewise failed to find a buyer owing to an inability to guarantee a consistent grade, despite its high (sometimes ca. 1 %) silver content.
The orebodies were compact and vugs, even of calcite, scarce. However, a few dozen small specimens of bright yellow sphalerite crystals were recovered from one small area (Panel 18) in the Main Zone (North). Most Lisheen sphalerite was dark treacle brown, and good crystallised specimens are very rare.
The Lisheen deposit is situated in the southern Irish Zn-Pb orefield, was the second largest mined Zn-Pb deposit in Ireland, with the resource (23 Mt @ 13.3 % Zn and 2.3 % Pb) mined from 1999 until 2015. At Lisheen, mineralisation is predominantly hosted by the Waulsortian Limestone Formation, which has been the focus of most published research. However, while minor, significant resources are located in the LOM of the underlying Ballysteen Formation, with notable Cu-Ni associations. The deposit contained six stratabound orebodies: Main Zone, Derryville, Bog East, Bog Central, Bog West and the Island Pod. Additional subeconomic mineralisation has been discovered at Barnalisheen to the northwest, and at Templetouhy and Bawnmore further east.
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Standard Detailed Gallery Strunz Chemical ElementsCommodity 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-localities35 valid minerals.
Rock Types Recorded
Rock list contains entries from the region specified including sub-localities
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Alphabetical List Tree DiagramDetailed Mineral List:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Stromeyerite | 2.BA.40 | AgCuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Renierite | 2.CB.35a | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| ⓘ | Nickeline | 2.CC.05 | NiAs |
| ⓘ | Millerite | 2.CC.20 | NiS |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Siegenite | 2.DA.05 | CoNi2S4 |
| ⓘ | Pyrite var. Bravoite | 2.EB.05a | (Fe,Ni)S2 |
| ⓘ | 2.EB.05a | FeS2 | |
| ⓘ | Vaesite | 2.EB.05a | NiS2 |
| ⓘ | Pyrite var. Arsenic-bearing Pyrite | 2.EB.05a | Fe(S,As)2 |
| ⓘ | Marcasite | 2.EB.10a | FeS2 |
| ⓘ | Pararammelsbergite | 2.EB.10e | NiAs2 |
| ⓘ | Rammelsbergite ? | 2.EB.15a | NiAs2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | Cobaltite | 2.EB.25 | CoAsS |
| ⓘ | Gersdorffite | 2.EB.25 | NiAsS |
| ⓘ | Ullmannite | 2.EB.25 | NiSbS |
| ⓘ | Bournonite | 2.GA.50 | PbCuSbS3 |
| ⓘ | Seligmannite | 2.GA.50 | PbCuAsS3 |
| ⓘ | 'Tennantite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)As4S12S |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| ⓘ | Tennantite-(Zn) | 2.GB.05 | Cu6(Cu4Zn2)As4S12S |
| ⓘ | Boulangerite | 2.HC.15 | Pb5Sb4S11 |
| ⓘ | Jordanite | 2.JB.30a | Pb14As6S23 |
| ⓘ | Gratonite | 2.JB.55 | Pb9As4S15 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Siderite | 5.AB.05 | FeCO3 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| ⓘ | Azurite ? | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Baryte | 7.AD.35 | BaSO4 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Annabergite | 8.CE.40 | Ni3(AsO4)2 · 8H2O |
| ⓘ | Pharmacolite | 8.CJ.50 | Ca(HAsO4) · 2H2O |
| Group 9 - Silicates | |||
| ⓘ | Muscovite var. Illite | 9.EC.15 | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| ⓘ | 9.EC.15 | KAl2(AlSi3O10)(OH)2 | |
| Unclassified | |||
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Serpentine Subgroup' | - | D3[Si2O5](OH)4 |
| ⓘ | 'Tetrahedrite Group' | - | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| ⓘ | 'Micrite' | - | |
| ⓘ | 'Sparite' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Annabergite | Ni3(AsO4)2 · 8H2O |
| H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Pharmacolite | Ca(HAsO4) · 2H2O |
| H | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| C | Carbon | |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | ⓘ Siderite | FeCO3 |
| O | Oxygen | |
| O | ⓘ Annabergite | Ni3(AsO4)2 · 8H2O |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Baryte | BaSO4 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Pharmacolite | Ca(HAsO4) · 2H2O |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Siderite | FeCO3 |
| O | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| Mg | Magnesium | |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Al | Aluminium | |
| Al | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Serpentine Subgroup | D3[Si2O5](OH)4 |
| S | Sulfur | |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Baryte | BaSO4 |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Boulangerite | Pb5Sb4S11 |
| S | ⓘ Bournonite | PbCuSbS3 |
| S | ⓘ Pyrite var. Bravoite | (Fe,Ni)S2 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Cobaltite | CoAsS |
| S | ⓘ Galena | PbS |
| S | ⓘ Gersdorffite | NiAsS |
| S | ⓘ Gratonite | Pb9As4S15 |
| S | ⓘ Jordanite | Pb14As6S23 |
| S | ⓘ Marcasite | FeS2 |
| S | ⓘ Millerite | NiS |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Renierite | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| S | ⓘ Seligmannite | PbCuAsS3 |
| S | ⓘ Siegenite | CoNi2S4 |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Stromeyerite | AgCuS |
| S | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| S | ⓘ Ullmannite | NiSbS |
| S | ⓘ Vaesite | NiS2 |
| S | ⓘ Pyrite var. Arsenic-bearing Pyrite | Fe(S,As)2 |
| S | ⓘ Tetrahedrite Group | M2(A6)M1(B4 C2)X3(D4)S1(Y12)S2(Z) |
| S | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| K | Potassium | |
| K | ⓘ Muscovite var. Illite | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Pharmacolite | Ca(HAsO4) · 2H2O |
| Fe | Iron | |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Pyrite var. Bravoite | (Fe,Ni)S2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Marcasite | FeS2 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Renierite | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| Fe | ⓘ Siderite | FeCO3 |
| Fe | ⓘ Pyrite var. Arsenic-bearing Pyrite | Fe(S,As)2 |
| Co | Cobalt | |
| Co | ⓘ Cobaltite | CoAsS |
| Co | ⓘ Siegenite | CoNi2S4 |
| Ni | Nickel | |
| Ni | ⓘ Annabergite | Ni3(AsO4)2 · 8H2O |
| Ni | ⓘ Pyrite var. Bravoite | (Fe,Ni)S2 |
| Ni | ⓘ Gersdorffite | NiAsS |
| Ni | ⓘ Millerite | NiS |
| Ni | ⓘ Nickeline | NiAs |
| Ni | ⓘ Pararammelsbergite | NiAs2 |
| Ni | ⓘ Rammelsbergite | NiAs2 |
| Ni | ⓘ Siegenite | CoNi2S4 |
| Ni | ⓘ Ullmannite | NiSbS |
| Ni | ⓘ Vaesite | NiS2 |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Bournonite | PbCuSbS3 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Cu | ⓘ Renierite | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| Cu | ⓘ Seligmannite | PbCuAsS3 |
| Cu | ⓘ Stromeyerite | AgCuS |
| Cu | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Cu | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| Zn | Zinc | |
| Zn | ⓘ Renierite | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| Zn | ⓘ Sphalerite | ZnS |
| Zn | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| Ge | Germanium | |
| Ge | ⓘ Renierite | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| As | Arsenic | |
| As | ⓘ Annabergite | Ni3(AsO4)2 · 8H2O |
| As | ⓘ Arsenopyrite | FeAsS |
| As | ⓘ Cobaltite | CoAsS |
| As | ⓘ Gersdorffite | NiAsS |
| As | ⓘ Gratonite | Pb9As4S15 |
| As | ⓘ Jordanite | Pb14As6S23 |
| As | ⓘ Nickeline | NiAs |
| As | ⓘ Pararammelsbergite | NiAs2 |
| As | ⓘ Pharmacolite | Ca(HAsO4) · 2H2O |
| As | ⓘ Rammelsbergite | NiAs2 |
| As | ⓘ Renierite | (Cu+,Zn)11Fe4(Ge4+,As5+)2S16 |
| As | ⓘ Seligmannite | PbCuAsS3 |
| As | ⓘ Tennantite Subgroup | Cu6(Cu4C22+)As4S12S |
| As | ⓘ Pyrite var. Arsenic-bearing Pyrite | Fe(S,As)2 |
| As | ⓘ Tennantite-(Zn) | Cu6(Cu4Zn2)As4S12S |
| Ag | Silver | |
| Ag | ⓘ Stromeyerite | AgCuS |
| Sb | Antimony | |
| Sb | ⓘ Boulangerite | Pb5Sb4S11 |
| Sb | ⓘ Bournonite | PbCuSbS3 |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Sb | ⓘ Ullmannite | NiSbS |
| Ba | Barium | |
| Ba | ⓘ Baryte | BaSO4 |
| Pb | Lead | |
| Pb | ⓘ Boulangerite | Pb5Sb4S11 |
| Pb | ⓘ Bournonite | PbCuSbS3 |
| Pb | ⓘ Galena | PbS |
| Pb | ⓘ Gratonite | Pb9As4S15 |
| Pb | ⓘ Jordanite | Pb14As6S23 |
| Pb | ⓘ Seligmannite | PbCuAsS3 |
Localities in this Region
- Munster
- Tipperary County
- Moyne
- Lisheen mine
- Moyne
- Tipperary County
Other Regions, Features and Areas containing this locality
British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
- AvaloniaVolcanic Arc
EuropeContinent
Ireland (island)Island
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References
Hitzman, M. W., Redmond, P. B., Beaty, D. W. (2002) The Carbonate-Hosted Lisheen Zn-Pb-Ag Deposit, County Tipperary, Ireland. Economic Geology, 97 (8) 1627-1655 doi:10.2113/gsecongeo.97.8.1627
Wilkinson, J. J., Eyre, S. L., Boyce, A. J. (2005) Ore-Forming Processes in Irish-Type Carbonate-Hosted Zn-Pb Deposits: Evidencefrom Mineralogy, Chemistry, and Isotopic Composition of Sulfides at the LisheenMine. Economic Geology, 100 (1) 63-86 doi:10.2113/100.1.0063
Pannalal, S. J., Symons, D. T. A., Sangster, D. F. (2008) Paleomagnetic Evidence for an Early Permian Age of the Lisheen Zn-Pb Deposit, Ireland. Economic Geology, 103 (8) 1641-1655 doi:10.2113/gsecongeo.103.8.1641
Yesares, Lola, Drummond, Drew A., Hollis, Steven P., Doran, Aileen L., Menuge, Julian F., Boyce, Adrian J., Blakeman, Robert J., Ashton, John H. (2019) Coupling Mineralogy, Textures, Stable and Radiogenic Isotopes in Identifying Ore-Forming Processes in Irish-Type Carbonate-Hosted Zn–Pb Deposits. Minerals, 9 (6) 335 doi:10.3390/min9060335
Frenzel, Max, Röhner, Markus, Cook, Nigel J., Gilbert, Sarah, Ciobanu, Cristiana L., Güven, John F. (2025) Mineralogy, mineral chemistry, and genesis of Cu-Ni-As-rich ores at Lisheen, Ireland. Mineralium Deposita, 60 (1). doi:10.1007/s00126-024-01299-8
[1]Doran, Aileen L.; Hollis, Steven P.; Menuge, Julian F.; Lyons, Connor; Piercey, Stephen J.; Boyce, Adrian J.; Slezak, Paul; Torremans, Koen; Güven, John (2025) Evidence for metal sources, fluid-mixing processes, and S isotope recycling within the feeder zone of an Irish type Zn-Pb deposit. Ore Geology Reviews, 182. 106660 doi:10.1016/j.oregeorev.2025.106660







Lisheen mine, Moyne, Tipperary County, Munster, Ireland