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Pestarena gold mine (Pestarena Mines), Macugnaga, Verbano-Cusio-Ossola Province, Piedmont, Italyi
Regional Level Types
Pestarena gold mine (Pestarena Mines)Mine
MacugnagaCommune
Verbano-Cusio-Ossola ProvinceProvince
PiedmontRegion
ItalyCountry

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Latitude & Longitude (WGS84):
45° North , 7° East (est.)
Estimate based on other nearby localities or region boundaries.
Margin of Error:
~8km
Type:
Köppen climate type:
Mindat Locality ID:
48172
Long-form identifier:
mindat:1:2:48172:1
GUID (UUID V4):
0
Name(s) in local language(s):
Miniera d'oro di Pestarena (Miniere di Pestarena), Macugnaga/Ceppo Morelli, Valle Anzasca, Val d'Ossola, Provincia del Verbano-Cusio-Ossola, Piemonte, Italia


Pestarena, the most important historical gold mine complex in the Alps, is located in Macugnaga and Ceppo Morelli municipalities.

This mine site interests an area of 4 km2 through about 40 km of tunnels on 15 main exploitation levels. The orebodies are composed of gold-bearing post-metamorphic structures, represented by mineralised cataclasites and veins, often discontinuous and with complex structural geometry. Gold mineralisation is hosted by the Monte Rosa Unit, comprising a sequence of paragneisses and micaschists with minor amphibolites, overlain by an orthogneisses unit. The Pestarena mine is developed within the paragneisses and micaschists, while in the adjacent Lavanchetto property, east of Pestarena and part of the Pestarena mining concession, the gold mineralisation occurs within the overlying orthogneisses. Depending on the host-rock lithology, the ore bodies show strongly different features: they occur along fractures and shear zones crosscutting the foliation at high angle within the hard orthogneiss unit, while are sub-parallel to the foliation within the micaschists and paragneisses (Stella, 1943). Particularly, at the Pestarena mine gold occurs along cataclastic bands and extensional veins mostly oriented WNW-ESE. Veins mineralogy is dominated by quartz, with subordinate carbonates, sericite, chlorite, tourmaline, rutile, apatite, and amphibole. Metallic minerals are typically pyrite and arsenopyrite, with minor pyrrhotite, sphalerite, galena, chalcopyrite, and tetrahedrite. Gold is invariably associated with sulfides, mainly with pyrite and galena.

In the second half of the 19th century the variously owned mines (generically Pestarena mines), which were intensively exploited since the 18th century (Nicolis de Robilant, 1784-85; Amoretti, 1794; De Saussure, 1796; Barelli, 1835), became sections of a larger British enterprise, "The Pestarena United Gold Mining Comany Ltd.". The most known of them are named: Acquavite, Cavone, Morghen, Peschiera, Pozzone-Speranza, Scarpia, Trappola. In 1902 the ownership passed from the British enterprise to the Italian company Pietro Maria Ceretti of Villadossola. In 1938 the mining complex was nationalised and transferred to the state-owned mining company Azienda Minerali Metallici Italiani (AMMI). In 1951 the Italian state granted to AMMI a mining concession, containing the Pestarena and Lavanchetto properties, valid until 2040. The old workings at Pestarena focused on exploiting the easiest (and highest-grade) portions. Gold-bearing ore was also extracted from other veins of the Pestarena mining concession, i.e. the veins Lavanchetto, Fornale, and Caccia, located at higher elevations E-SE of Pestarena. After World War II, however, production costs continued to grow as gold grade declined. Consequently, the mine was abandoned in 1961, leaving approximately 300,000 tons of ore at site with a gold content of at least 7 g/t. In recent times, the company Miniere di Pestarena S.r.l. has taken over the mining concession (which includes also the adjacent Lavanchetto property) and plans to re-evaluate and potentially reopen the mine.

Pestarena mine, in the true sense of the word, includes underground workings between elevation 700 and 1031 m a.s.l. and consists of three main NW-SW-trending mineralised veins, named "Liz", "Quarzo", and "Uno" (De Angelis, 2003). The ore bodies are accessed through two ways: one, the main decline, starts from Pestarena village (Macugnaga municipality) at 1031 m and descends to 700 m, the other, the Morghen haulage level (2300 m long and equipped with mining electrical rail) starts from 870 m and connects the exploitation levels with the ore processing facility at Ceppo Morelli, which now lies abandoned.

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


25 valid minerals.

Detailed Mineral List:

ⓘ Acanthite ?
Formula: Ag2S
ⓘ 'Amphibole Supergroup'
Formula: AB2C5(T8O22)W2
ⓘ Ankerite
Formula: Ca(Fe2+,Mg)(CO3)2
ⓘ 'Apatite'
Formula: Ca5(PO4)3A
ⓘ Aragonite
Formula: CaCO3
ⓘ Arsenopyrite
Formula: FeAsS
References:
ⓘ Bismuthinite ?
Formula: Bi2S3
Description: As "Wismuthglanz" (a German name used in the past not only for bismuthinite, but also for emplectite and other Bi minerals)
ⓘ Calcite
Formula: CaCO3
References:
ⓘ Chalcopyrite
Formula: CuFeS2
References:
ⓘ 'Chlorite Group'
ⓘ Dolomite
Formula: CaMg(CO3)2
ⓘ Emplectite
Formula: CuBiS2
ⓘ Galena
Formula: PbS
References:
ⓘ Graphite
Formula: C
ⓘ Hydrozincite
Formula: Zn5(CO3)2(OH)6
ⓘ 'Limonite'
ⓘ Magnesite
Formula: MgCO3
ⓘ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
ⓘ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
ⓘ Native Bismuth
Formula: Bi
ⓘ Native Gold
Formula: Au
References:
ⓘ Pickeringite
Formula: MgAl2(SO4)4 · 22H2O
ⓘ Pyrargyrite
Formula: Ag3SbS3
ⓘ Pyrite
Formula: FeS2
References:
ⓘ Pyrrhotite
Formula: Fe1-xS
ⓘ Quartz
Formula: SiO2
References:
ⓘ Rutile
Formula: TiO2
ⓘ Scheelite
Formula: Ca(WO4)
ⓘ Siderite
Formula: FeCO3
ⓘ Sphalerite
Formula: ZnS
ⓘ 'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
ⓘ 'Tourmaline'
Formula: AD3G6(T6O18)(BO3)3X3Z

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Gold1.AA.05Au
ⓘNative Bismuth1.CA.05Bi
ⓘGraphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
ⓘAcanthite ?2.BA.35Ag2S
ⓘSphalerite2.CB.05aZnS
ⓘChalcopyrite2.CB.10aCuFeS2
ⓘPyrrhotite2.CC.10Fe1-xS
ⓘGalena2.CD.10PbS
ⓘBismuthinite ?2.DB.05Bi2S3
ⓘPyrite2.EB.05aFeS2
ⓘArsenopyrite2.EB.20FeAsS
ⓘPyrargyrite2.GA.05Ag3SbS3
ⓘ'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
ⓘEmplectite2.HA.05CuBiS2
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2
ⓘRutile4.DB.05TiO2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘMagnesite5.AB.05MgCO3
ⓘSiderite5.AB.05FeCO3
ⓘAnkerite5.AB.10Ca(Fe2+,Mg)(CO3)2
ⓘDolomite5.AB.10CaMg(CO3)2
ⓘAragonite5.AB.15CaCO3
ⓘHydrozincite5.BA.15Zn5(CO3)2(OH)6
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘPickeringite7.CB.85MgAl2(SO4)4 · 22H2O
ⓘScheelite7.GA.05Ca(WO4)
Group 9 - Silicates
ⓘMuscovite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘvar. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
ⓘ'Amphibole Supergroup'-AB2C5(T8O22)W2
ⓘ'Chlorite Group'-
ⓘ'Limonite'-
ⓘ'Tourmaline'-AD3G6(T6O18)(BO3)3X3Z
ⓘ'Apatite'-Ca5(PO4)3A

List of minerals for each chemical element

HHydrogen
Hⓘ HydrozinciteZn5(CO3)2(OH)6
Hⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Hⓘ PickeringiteMgAl2(SO4)4 · 22H2O
Hⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
BBoron
Bⓘ TourmalineAD3G6(T6O18)(BO3)3X3Z
CCarbon
Cⓘ AnkeriteCa(Fe2+,Mg)(CO3)2
Cⓘ AragoniteCaCO3
Cⓘ CalciteCaCO3
Cⓘ DolomiteCaMg(CO3)2
Cⓘ GraphiteC
Cⓘ HydrozinciteZn5(CO3)2(OH)6
Cⓘ MagnesiteMgCO3
Cⓘ SideriteFeCO3
OOxygen
Oⓘ Amphibole SupergroupAB2C5(T8O22)W2
Oⓘ AnkeriteCa(Fe2+,Mg)(CO3)2
Oⓘ AragoniteCaCO3
Oⓘ CalciteCaCO3
Oⓘ DolomiteCaMg(CO3)2
Oⓘ HydrozinciteZn5(CO3)2(OH)6
Oⓘ MagnesiteMgCO3
Oⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Oⓘ PickeringiteMgAl2(SO4)4 · 22H2O
Oⓘ QuartzSiO2
Oⓘ RutileTiO2
Oⓘ ScheeliteCa(WO4)
Oⓘ SideriteFeCO3
Oⓘ TourmalineAD3G6(T6O18)(BO3)3X3Z
Oⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oⓘ ApatiteCa5(PO4)3A
MgMagnesium
Mgⓘ AnkeriteCa(Fe2+,Mg)(CO3)2
Mgⓘ DolomiteCaMg(CO3)2
Mgⓘ MagnesiteMgCO3
Mgⓘ PickeringiteMgAl2(SO4)4 · 22H2O
AlAluminium
Alⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Alⓘ PickeringiteMgAl2(SO4)4 · 22H2O
Alⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Siⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Siⓘ QuartzSiO2
Siⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
PPhosphorus
Pⓘ ApatiteCa5(PO4)3A
SSulfur
Sⓘ AcanthiteAg2S
Sⓘ ArsenopyriteFeAsS
Sⓘ BismuthiniteBi2S3
Sⓘ ChalcopyriteCuFeS2
Sⓘ EmplectiteCuBiS2
Sⓘ GalenaPbS
Sⓘ PickeringiteMgAl2(SO4)4 · 22H2O
Sⓘ PyrargyriteAg3SbS3
Sⓘ PyriteFeS2
Sⓘ PyrrhotiteFe1-xS
Sⓘ SphaleriteZnS
Sⓘ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
KPotassium
Kⓘ MuscoviteKAl2(AlSi3O10)(OH)2
Kⓘ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Caⓘ AnkeriteCa(Fe2+,Mg)(CO3)2
Caⓘ AragoniteCaCO3
Caⓘ CalciteCaCO3
Caⓘ DolomiteCaMg(CO3)2
Caⓘ ScheeliteCa(WO4)
Caⓘ ApatiteCa5(PO4)3A
TiTitanium
Tiⓘ RutileTiO2
FeIron
Feⓘ AnkeriteCa(Fe2+,Mg)(CO3)2
Feⓘ ArsenopyriteFeAsS
Feⓘ ChalcopyriteCuFeS2
Feⓘ PyriteFeS2
Feⓘ PyrrhotiteFe1-xS
Feⓘ SideriteFeCO3
CuCopper
Cuⓘ ChalcopyriteCuFeS2
Cuⓘ EmplectiteCuBiS2
Cuⓘ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Znⓘ HydrozinciteZn5(CO3)2(OH)6
Znⓘ SphaleriteZnS
AsArsenic
Asⓘ ArsenopyriteFeAsS
AgSilver
Agⓘ AcanthiteAg2S
Agⓘ PyrargyriteAg3SbS3
SbAntimony
Sbⓘ PyrargyriteAg3SbS3
Sbⓘ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
WTungsten
Wⓘ ScheeliteCa(WO4)
AuGold
Auⓘ Native GoldAu
PbLead
Pbⓘ GalenaPbS
BiBismuth
Biⓘ Native BismuthBi
Biⓘ BismuthiniteBi2S3
Biⓘ EmplectiteCuBiS2

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate
  • AlpsAccretionary Complex
EuropeContinent
Italy

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