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Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France i
Regional Level Types
Sankt Jakob Mine Mine
Saint Jacques vein Vein
Neuenberg Group of Veins
Sainte-Marie-aux-Mines Commune
Colmar-Ribeauvillé Arrondissement
Haut-Rhin Department
Grand Est Region
France Country

Regional Level Types
Sankt Jakob Mine	Mine
Saint Jacques vein	Vein
Neuenberg	Group of Veins
Sainte-Marie-aux-Mines	Commune
Colmar-Ribeauvillé	Arrondissement
Haut-Rhin	Department
Grand Est	Region
France	Country

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Predictive Mineralogy

Flos Ferri

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Native Arsenic

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Chalcopyrite, etc.

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Flos Ferri

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Native Arsenic

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Chalcopyrite, etc.

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Flos Ferri

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Native Arsenic

Sankt Jakob Mine, Saint Jacques vein, Neuenberg, Sainte-Marie-aux-Mines, Colmar-Ribeauvillé, Haut-Rhin, Grand Est, France

Type:

Mine

Mindat Locality ID:

21913

Long-form identifier:

mindat:1:2:21913:3

GUID (UUID V4):

Other/historical names associated with this locality:

Alsace

Name(s) in local language(s):

Mine St Jacques (Grube Jakob), Sainte-Marie-aux-Mines, Haut-Rhin, Alsace, France

Upper and lower Sankt-Jacob mine are known.

As this locality lies in the Sainte-Marie-aux-Mines district, the place is protected by a archaeological mining district status and all collecting is prohibited.

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.

ⓘ Silver

Mineral List

ⓘ 'Tennantite Subgroup'

ⓘ 'Tetrahedrite Subgroup'

ⓘ Weilite

ⓘ Wittichenite

ⓘ Xanthoconite

76 valid minerals. 1 erroneous literature entry.

Detailed Mineral List:

ⓘ Acanthite

Formula: Ag₂S

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Aikinite

Formula: CuPbBiS₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Ankerite

Formula: Ca(Fe²⁺,Mg)(CO₃)₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Annabergite

Formula: Ni₃(AsO₄)₂ · 8H₂O

References:

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Aragonite

Formula: CaCO₃

References:

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Aragonite var. Flos Ferri

Formula: CaCO₃

References:

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Aramayoite

Formula: Ag₃Sb₂(Bi,Sb)S₆

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Argentopyrite

Formula: AgFe₂S₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ ~~Arsenolamprite~~

Formula: As

Description: Bari mentions in his study that arsenolamprite was never found in all the specimens he analysed.

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Arsenolite

Formula: As₂O₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Arsenopyrite

Formula: FeAsS

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Baumstarkite

Formula: Ag₃Sb₃S₆

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Berryite

Formula: Cu₃Ag₂Pb₃Bi₇S₁₆

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Bismuthinite

Formula: Bi₂S₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Bournonite

Formula: PbCuSbS₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Calcite

Formula: CaCO₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Chalcopyrite

Formula: CuFeS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Chlorargyrite

Formula: AgCl

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Cornubite

Formula: Cu₅(AsO₄)₂(OH)₄

References:

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Cosalite

Formula: Pb₂Bi₂S₅

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Cubanite

Formula: CuFe₂S₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Dervillite

Formula: Ag₂AsS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Dolomite

Formula: CaMg(CO₃)₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Dyscrasite

Formula: Ag₃Sb

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Emplectite

Formula: CuBiS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Ferrarisite

Formula: Ca₅(AsO₄)₂(HAsO₄)₂ · 9H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Fluckite

Formula: CaMn²⁺(AsO₃OH)₂ · 2H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Galena

Formula: PbS

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Giftgrubeite

Formula: CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Guérinite

Formula: Ca₆(HAsO₄)₃(AsO₄)₂ · 10.5H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Gypsum

Formula: CaSO₄ · 2H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Haidingerite

Formula: CaHAsO₄ · H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Hematite

Formula: Fe₂O₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Hörnesite

Formula: Mg₃(AsO₄)₂ · 8H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Kaolinite

Formula: Al₂(Si₂O₅)(OH)₄

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Kobellite

Formula: Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Lautite

Formula: CuAsS

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ 'Limonite'

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Löllingite

Formula: FeAs₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Malachite

Formula: Cu₂(CO₃)(OH)₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Marcasite

Formula: FeS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Matildite

Formula: AgBiS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Mcnearite

Formula: NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Miargyrite

Formula: AgSbS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Mimetite

Formula: Pb₅(AsO₄)₃Cl

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Mirabilite

Formula: Na₂SO₄ · 10H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Native Arsenic

Formula: As

References:

Mineralogical Museum of the City : Sainte Marie aux Mines

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Native Bismuth

Formula: Bi

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Native Silver

Formula: Ag

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Nickeline

Formula: NiAs

References:

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Nickelskutterudite

Formula: NiAs₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Orpiment

Formula: As₂S₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Orthoserpierite

Formula: Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Pararammelsbergite

Formula: NiAs₂

References:

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Pavonite

Formula: AgBi₃S₅

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Pearceite

Formula: [Ag₆As₂S₇][Ag₉CuS₄]

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Pharmacolite

Formula: Ca(HAsO₄) · 2H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Phaunouxite

Formula: Ca₃(AsO₄)₂ · 11H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Picropharmacolite

Formula: Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Polybasite

Formula: [Ag₆Sb₂S₇][Ag₉CuS₄]

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Proustite

Formula: Ag₃AsS₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

✪ Pyrargyrite

Formula: Ag₃SbS₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Pyrite

Formula: FeS₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Pyromorphite

Formula: Pb₅(PO₄)₃Cl

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Quartz

Formula: SiO₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Quartz var. Chalcedony

Formula: SiO₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Rammelsbergite

Formula: NiAs₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

Wittern, A.; Journée, J.R. (1997) Mineralien finden in den Vogesen. Verlag Sven von Loga. 160 pp.

ⓘ Rauenthalite

Formula: Ca₃(AsO₄)₂ · 10H₂O

References:

in the collection of Joachim Esche

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Realgar

Formula: As₄S₄

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Rösslerite

Formula: Mg(HAsO₄) · 7H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Safflorite

Formula: (Co,Ni,Fe)As₂

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Sainfeldite

Formula: Ca₅(AsO₄)₂(AsO₃OH)₂ · 4H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Scorodite

Formula: Fe³⁺AsO₄ · 2H₂O

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Semseyite

Formula: Pb₉Sb₈S₂₁

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Siderite

Formula: FeCO₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Skutterudite

Formula: CoAs₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Sphalerite

Formula: ZnS

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ 'Tennantite Subgroup'

Formula: Cu₆(Cu₄C²⁺₂)As₄S₁₂S

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ 'Tetrahedrite Subgroup'

Formula: Cu₆(Cu₄C²⁺₂)Sb₄S₁₂S

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Weilite

Formula: Ca(HAsO₄)

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Wittichenite

Formula: Cu₃BiS₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

ⓘ Xanthoconite

Formula: Ag₃AsS₃

References:

This mine worked the same vein as Gabe gottes mine.

From the 19th century, ore from a large part of the Saint-Jacques mine network was transported to level -40 of Gabe Gottes before being sent to the processing plant.

The mineralization of this sector is therefore very comparable to that of tje Gabe Gottes mine.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘ	Native Silver	1.AA.05	Ag
ⓘ	Native Arsenic	1.CA.05	As
ⓘ	Native Bismuth	1.CA.05	Bi
ⓘ	Arsenolamprite ?	1.CA.10	As
Group 2 - Sulphides and Sulfosalts
ⓘ	Dyscrasite	2.AA.35	Ag₃Sb
ⓘ	Acanthite	2.BA.35	Ag₂S
ⓘ	Sphalerite	2.CB.05a	ZnS
ⓘ	Chalcopyrite	2.CB.10a	CuFeS₂
ⓘ	Lautite	2.CB.40	CuAsS
ⓘ	Cubanite	2.CB.55a	CuFe₂S₃
ⓘ	Argentopyrite	2.CB.65	AgFe₂S₃
ⓘ	Nickeline	2.CC.05	NiAs
ⓘ	Galena	2.CD.10	PbS
ⓘ	Bismuthinite	2.DB.05	Bi₂S₃
ⓘ	Pyrite	2.EB.05a	FeS₂
ⓘ	Marcasite	2.EB.10a	FeS₂
ⓘ	Pararammelsbergite	2.EB.10e	NiAs₂
ⓘ	Löllingite	2.EB.15a	FeAs₂
ⓘ	Rammelsbergite	2.EB.15a	NiAs₂
ⓘ	Safflorite	2.EB.15a	(Co,Ni,Fe)As₂
ⓘ	Arsenopyrite	2.EB.20	FeAsS
ⓘ	Nickelskutterudite	2.EC.05	NiAs₃
ⓘ	Skutterudite	2.EC.05	CoAs₃
ⓘ	Realgar	2.FA.15a	As₄S₄
ⓘ	Orpiment	2.FA.30	As₂S₃
ⓘ	Proustite	2.GA.05	Ag₃AsS₃
ⓘ	Pyrargyrite	2.GA.05	Ag₃SbS₃
ⓘ	Xanthoconite	2.GA.10	Ag₃AsS₃
ⓘ	Wittichenite	2.GA.20	Cu₃BiS₃
ⓘ	Bournonite	2.GA.50	PbCuSbS₃
ⓘ	'Tennantite Subgroup'	2.GB.05	Cu₆(Cu₄C²⁺₂)As₄S₁₂S
ⓘ	'Tetrahedrite Subgroup'	2.GB.05	Cu₆(Cu₄C²⁺₂)Sb₄S₁₂S
ⓘ	Pearceite	2.GB.15	[Ag₆As₂S₇][Ag₉CuS₄]
ⓘ	Polybasite	2.GB.15	[Ag₆Sb₂S₇][Ag₉CuS₄]
ⓘ	Emplectite	2.HA.05	CuBiS₂
ⓘ	Miargyrite	2.HA.10	AgSbS₂
ⓘ	Aramayoite	2.HA.25	Ag₃Sb₂(Bi,Sb)S₆
ⓘ	Baumstarkite	2.HA.25	Ag₃Sb₃S₆
ⓘ	Aikinite	2.HB.05a	CuPbBiS₃
ⓘ	Kobellite	2.HB.10a	Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉
ⓘ	Berryite	2.HB.20d	Cu₃Ag₂Pb₃Bi₇S₁₆
ⓘ	Semseyite	2.HC.10d	Pb₉Sb₈S₂₁
ⓘ	Pavonite	2.JA.05a	AgBi₃S₅
ⓘ	Matildite	2.JA.20	AgBiS₂
ⓘ	Cosalite	2.JB.10	Pb₂Bi₂S₅
ⓘ	Dervillite	2.LA.10	Ag₂AsS₂
Group 3 - Halides
ⓘ	Chlorargyrite	3.AA.15	AgCl
Group 4 - Oxides and Hydroxides
ⓘ	Hematite	4.CB.05	Fe₂O₃
ⓘ	Arsenolite	4.CB.50	As₂O₃
ⓘ	Quartz var. Chalcedony	4.DA.05	SiO₂
ⓘ		4.DA.05	SiO₂
Group 5 - Nitrates and Carbonates
ⓘ	Calcite	5.AB.05	CaCO₃
ⓘ	Siderite	5.AB.05	FeCO₃
ⓘ	Ankerite	5.AB.10	Ca(Fe²⁺,Mg)(CO₃)₂
ⓘ	Dolomite	5.AB.10	CaMg(CO₃)₂
ⓘ	Aragonite	5.AB.15	CaCO₃
ⓘ	var. Flos Ferri	5.AB.15	CaCO₃
ⓘ	Malachite	5.BA.10	Cu₂(CO₃)(OH)₂
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘ	Mirabilite	7.CD.10	Na₂SO₄ · 10H₂O
ⓘ	Gypsum	7.CD.40	CaSO₄ · 2H₂O
ⓘ	Orthoserpierite	7.DD.30	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
Group 8 - Phosphates, Arsenates and Vanadates
ⓘ	Weilite	8.AD.10	Ca(HAsO₄)
ⓘ	Cornubite	8.BD.30	Cu₅(AsO₄)₂(OH)₄
ⓘ	Mimetite	8.BN.05	Pb₅(AsO₄)₃Cl
ⓘ	Pyromorphite	8.BN.05	Pb₅(PO₄)₃Cl
ⓘ	Giftgrubeite	8.CB.10	CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O
ⓘ	Scorodite	8.CD.10	Fe³⁺AsO₄ · 2H₂O
ⓘ	Rösslerite	8.CE.20	Mg(HAsO₄) · 7H₂O
ⓘ	Annabergite	8.CE.40	Ni₃(AsO₄)₂ · 8H₂O
ⓘ	Hörnesite	8.CE.40	Mg₃(AsO₄)₂ · 8H₂O
ⓘ	Fluckite	8.CG.	CaMn²⁺(AsO₃OH)₂ · 2H₂O
ⓘ	Picropharmacolite	8.CH.15	Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O
ⓘ	Sainfeldite	8.CJ.	Ca₅(AsO₄)₂(AsO₃OH)₂ · 4H₂O
ⓘ	Haidingerite	8.CJ.20	CaHAsO₄ · H₂O
ⓘ	Ferrarisite	8.CJ.30	Ca₅(AsO₄)₂(HAsO₄)₂ · 9H₂O
ⓘ	Phaunouxite	8.CJ.40	Ca₃(AsO₄)₂ · 11H₂O
ⓘ	Rauenthalite	8.CJ.40	Ca₃(AsO₄)₂ · 10H₂O
ⓘ	Pharmacolite	8.CJ.50	Ca(HAsO₄) · 2H₂O
ⓘ	Mcnearite	8.CJ.55	NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O
ⓘ	Guérinite	8.CJ.75	Ca₆(HAsO₄)₃(AsO₄)₂ · 10.5H₂O
Group 9 - Silicates
ⓘ	Kaolinite	9.ED.05	Al₂(Si₂O₅)(OH)₄
Unclassified
ⓘ	'Limonite'	-

List of minerals for each chemical element

H	Hydrogen
H	ⓘ Annabergite	Ni₃(AsO₄)₂ · 8H₂O
H	ⓘ Cornubite	Cu₅(AsO₄)₂(OH)₄
H	ⓘ Ferrarisite	Ca₅(AsO₄)₂(HAsO₄)₂ · 9H₂O
H	ⓘ Fluckite	CaMn²⁺(AsO₃OH)₂ · 2H₂O
H	ⓘ Guérinite	Ca₆(HAsO₄)₃(AsO₄)₂ · 10.5H₂O
H	ⓘ Gypsum	CaSO₄ · 2H₂O
H	ⓘ Haidingerite	CaHAsO₄ · H₂O
H	ⓘ Hörnesite	Mg₃(AsO₄)₂ · 8H₂O
H	ⓘ Kaolinite	Al₂(Si₂O₅)(OH)₄
H	ⓘ Malachite	Cu₂(CO₃)(OH)₂
H	ⓘ Mcnearite	NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O
H	ⓘ Mirabilite	Na₂SO₄ · 10H₂O
H	ⓘ Orthoserpierite	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
H	ⓘ Pharmacolite	Ca(HAsO₄) · 2H₂O
H	ⓘ Phaunouxite	Ca₃(AsO₄)₂ · 11H₂O
H	ⓘ Picropharmacolite	Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O
H	ⓘ Rauenthalite	Ca₃(AsO₄)₂ · 10H₂O
H	ⓘ Rösslerite	Mg(HAsO₄) · 7H₂O
H	ⓘ Sainfeldite	Ca₅(AsO₄)₂(AsO₃OH)₂ · 4H₂O
H	ⓘ Scorodite	Fe³⁺AsO₄ · 2H₂O
H	ⓘ Weilite	Ca(HAsO₄)
H	ⓘ Giftgrubeite	CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O
C	Carbon
C	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
C	ⓘ Aragonite	CaCO₃
C	ⓘ Calcite	CaCO₃
C	ⓘ Dolomite	CaMg(CO₃)₂
C	ⓘ Malachite	Cu₂(CO₃)(OH)₂
C	ⓘ Siderite	FeCO₃
C	ⓘ Aragonite var. Flos Ferri	CaCO₃
O	Oxygen
O	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
O	ⓘ Annabergite	Ni₃(AsO₄)₂ · 8H₂O
O	ⓘ Arsenolite	As₂O₃
O	ⓘ Aragonite	CaCO₃
O	ⓘ Calcite	CaCO₃
O	ⓘ Quartz var. Chalcedony	SiO₂
O	ⓘ Cornubite	Cu₅(AsO₄)₂(OH)₄
O	ⓘ Dolomite	CaMg(CO₃)₂
O	ⓘ Ferrarisite	Ca₅(AsO₄)₂(HAsO₄)₂ · 9H₂O
O	ⓘ Fluckite	CaMn²⁺(AsO₃OH)₂ · 2H₂O
O	ⓘ Guérinite	Ca₆(HAsO₄)₃(AsO₄)₂ · 10.5H₂O
O	ⓘ Gypsum	CaSO₄ · 2H₂O
O	ⓘ Haidingerite	CaHAsO₄ · H₂O
O	ⓘ Hematite	Fe₂O₃
O	ⓘ Hörnesite	Mg₃(AsO₄)₂ · 8H₂O
O	ⓘ Kaolinite	Al₂(Si₂O₅)(OH)₄
O	ⓘ Malachite	Cu₂(CO₃)(OH)₂
O	ⓘ Mcnearite	NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O
O	ⓘ Mimetite	Pb₅(AsO₄)₃Cl
O	ⓘ Mirabilite	Na₂SO₄ · 10H₂O
O	ⓘ Orthoserpierite	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
O	ⓘ Pharmacolite	Ca(HAsO₄) · 2H₂O
O	ⓘ Phaunouxite	Ca₃(AsO₄)₂ · 11H₂O
O	ⓘ Picropharmacolite	Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O
O	ⓘ Pyromorphite	Pb₅(PO₄)₃Cl
O	ⓘ Quartz	SiO₂
O	ⓘ Rauenthalite	Ca₃(AsO₄)₂ · 10H₂O
O	ⓘ Rösslerite	Mg(HAsO₄) · 7H₂O
O	ⓘ Sainfeldite	Ca₅(AsO₄)₂(AsO₃OH)₂ · 4H₂O
O	ⓘ Scorodite	Fe³⁺AsO₄ · 2H₂O
O	ⓘ Siderite	FeCO₃
O	ⓘ Weilite	Ca(HAsO₄)
O	ⓘ Aragonite var. Flos Ferri	CaCO₃
O	ⓘ Giftgrubeite	CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O
Na	Sodium
Na	ⓘ Mcnearite	NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O
Na	ⓘ Mirabilite	Na₂SO₄ · 10H₂O
Mg	Magnesium
Mg	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
Mg	ⓘ Dolomite	CaMg(CO₃)₂
Mg	ⓘ Hörnesite	Mg₃(AsO₄)₂ · 8H₂O
Mg	ⓘ Picropharmacolite	Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O
Mg	ⓘ Rösslerite	Mg(HAsO₄) · 7H₂O
Al	Aluminium
Al	ⓘ Kaolinite	Al₂(Si₂O₅)(OH)₄
Si	Silicon
Si	ⓘ Quartz var. Chalcedony	SiO₂
Si	ⓘ Kaolinite	Al₂(Si₂O₅)(OH)₄
Si	ⓘ Quartz	SiO₂
P	Phosphorus
P	ⓘ Pyromorphite	Pb₅(PO₄)₃Cl
S	Sulfur
S	ⓘ Acanthite	Ag₂S
S	ⓘ Aikinite	CuPbBiS₃
S	ⓘ Argentopyrite	AgFe₂S₃
S	ⓘ Arsenopyrite	FeAsS
S	ⓘ Aramayoite	Ag₃Sb₂(Bi,Sb)S₆
S	ⓘ Berryite	Cu₃Ag₂Pb₃Bi₇S₁₆
S	ⓘ Bismuthinite	Bi₂S₃
S	ⓘ Bournonite	PbCuSbS₃
S	ⓘ Chalcopyrite	CuFeS₂
S	ⓘ Cosalite	Pb₂Bi₂S₅
S	ⓘ Cubanite	CuFe₂S₃
S	ⓘ Dervillite	Ag₂AsS₂
S	ⓘ Emplectite	CuBiS₂
S	ⓘ Galena	PbS
S	ⓘ Gypsum	CaSO₄ · 2H₂O
S	ⓘ Kobellite	Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉
S	ⓘ Lautite	CuAsS
S	ⓘ Marcasite	FeS₂
S	ⓘ Matildite	AgBiS₂
S	ⓘ Miargyrite	AgSbS₂
S	ⓘ Mirabilite	Na₂SO₄ · 10H₂O
S	ⓘ Orpiment	As₂S₃
S	ⓘ Orthoserpierite	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
S	ⓘ Pavonite	AgBi₃S₅
S	ⓘ Pearceite	[Ag₆As₂S₇][Ag₉CuS₄]
S	ⓘ Polybasite	[Ag₆Sb₂S₇][Ag₉CuS₄]
S	ⓘ Proustite	Ag₃AsS₃
S	ⓘ Pyrargyrite	Ag₃SbS₃
S	ⓘ Pyrite	FeS₂
S	ⓘ Realgar	As₄S₄
S	ⓘ Semseyite	Pb₉Sb₈S₂₁
S	ⓘ Sphalerite	ZnS
S	ⓘ Tennantite Subgroup	Cu₆(Cu₄C₂²⁺)As₄S₁₂S
S	ⓘ Tetrahedrite Subgroup	Cu₆(Cu₄C₂²⁺)Sb₄S₁₂S
S	ⓘ Wittichenite	Cu₃BiS₃
S	ⓘ Xanthoconite	Ag₃AsS₃
S	ⓘ Baumstarkite	Ag₃Sb₃S₆
Cl	Chlorine
Cl	ⓘ Chlorargyrite	AgCl
Cl	ⓘ Mimetite	Pb₅(AsO₄)₃Cl
Cl	ⓘ Pyromorphite	Pb₅(PO₄)₃Cl
Ca	Calcium
Ca	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
Ca	ⓘ Aragonite	CaCO₃
Ca	ⓘ Calcite	CaCO₃
Ca	ⓘ Dolomite	CaMg(CO₃)₂
Ca	ⓘ Ferrarisite	Ca₅(AsO₄)₂(HAsO₄)₂ · 9H₂O
Ca	ⓘ Fluckite	CaMn²⁺(AsO₃OH)₂ · 2H₂O
Ca	ⓘ Guérinite	Ca₆(HAsO₄)₃(AsO₄)₂ · 10.5H₂O
Ca	ⓘ Gypsum	CaSO₄ · 2H₂O
Ca	ⓘ Haidingerite	CaHAsO₄ · H₂O
Ca	ⓘ Mcnearite	NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O
Ca	ⓘ Orthoserpierite	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
Ca	ⓘ Pharmacolite	Ca(HAsO₄) · 2H₂O
Ca	ⓘ Phaunouxite	Ca₃(AsO₄)₂ · 11H₂O
Ca	ⓘ Picropharmacolite	Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O
Ca	ⓘ Rauenthalite	Ca₃(AsO₄)₂ · 10H₂O
Ca	ⓘ Sainfeldite	Ca₅(AsO₄)₂(AsO₃OH)₂ · 4H₂O
Ca	ⓘ Weilite	Ca(HAsO₄)
Ca	ⓘ Aragonite var. Flos Ferri	CaCO₃
Ca	ⓘ Giftgrubeite	CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O
Mn	Manganese
Mn	ⓘ Fluckite	CaMn²⁺(AsO₃OH)₂ · 2H₂O
Mn	ⓘ Giftgrubeite	CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O
Fe	Iron
Fe	ⓘ Ankerite	Ca(Fe²⁺,Mg)(CO₃)₂
Fe	ⓘ Argentopyrite	AgFe₂S₃
Fe	ⓘ Arsenopyrite	FeAsS
Fe	ⓘ Chalcopyrite	CuFeS₂
Fe	ⓘ Cubanite	CuFe₂S₃
Fe	ⓘ Hematite	Fe₂O₃
Fe	ⓘ Löllingite	FeAs₂
Fe	ⓘ Marcasite	FeS₂
Fe	ⓘ Pyrite	FeS₂
Fe	ⓘ Safflorite	(Co,Ni,Fe)As₂
Fe	ⓘ Scorodite	Fe³⁺AsO₄ · 2H₂O
Fe	ⓘ Siderite	FeCO₃
Co	Cobalt
Co	ⓘ Safflorite	(Co,Ni,Fe)As₂
Co	ⓘ Skutterudite	CoAs₃
Ni	Nickel
Ni	ⓘ Annabergite	Ni₃(AsO₄)₂ · 8H₂O
Ni	ⓘ Nickelskutterudite	NiAs₃
Ni	ⓘ Nickeline	NiAs
Ni	ⓘ Pararammelsbergite	NiAs₂
Ni	ⓘ Rammelsbergite	NiAs₂
Ni	ⓘ Safflorite	(Co,Ni,Fe)As₂
Cu	Copper
Cu	ⓘ Aikinite	CuPbBiS₃
Cu	ⓘ Berryite	Cu₃Ag₂Pb₃Bi₇S₁₆
Cu	ⓘ Bournonite	PbCuSbS₃
Cu	ⓘ Chalcopyrite	CuFeS₂
Cu	ⓘ Cornubite	Cu₅(AsO₄)₂(OH)₄
Cu	ⓘ Cubanite	CuFe₂S₃
Cu	ⓘ Emplectite	CuBiS₂
Cu	ⓘ Kobellite	Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉
Cu	ⓘ Lautite	CuAsS
Cu	ⓘ Malachite	Cu₂(CO₃)(OH)₂
Cu	ⓘ Orthoserpierite	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
Cu	ⓘ Pearceite	[Ag₆As₂S₇][Ag₉CuS₄]
Cu	ⓘ Polybasite	[Ag₆Sb₂S₇][Ag₉CuS₄]
Cu	ⓘ Tennantite Subgroup	Cu₆(Cu₄C₂²⁺)As₄S₁₂S
Cu	ⓘ Tetrahedrite Subgroup	Cu₆(Cu₄C₂²⁺)Sb₄S₁₂S
Cu	ⓘ Wittichenite	Cu₃BiS₃
Zn	Zinc
Zn	ⓘ Orthoserpierite	Ca(Cu,Zn)₄(SO₄)₂(OH)₆ · 3H₂O
Zn	ⓘ Sphalerite	ZnS
As	Arsenic
As	ⓘ Annabergite	Ni₃(AsO₄)₂ · 8H₂O
As	ⓘ Arsenolite	As₂O₃
As	ⓘ Arsenopyrite	FeAsS
As	ⓘ Arsenolamprite	As
As	ⓘ Native Arsenic	As
As	ⓘ Cornubite	Cu₅(AsO₄)₂(OH)₄
As	ⓘ Dervillite	Ag₂AsS₂
As	ⓘ Ferrarisite	Ca₅(AsO₄)₂(HAsO₄)₂ · 9H₂O
As	ⓘ Fluckite	CaMn²⁺(AsO₃OH)₂ · 2H₂O
As	ⓘ Guérinite	Ca₆(HAsO₄)₃(AsO₄)₂ · 10.5H₂O
As	ⓘ Haidingerite	CaHAsO₄ · H₂O
As	ⓘ Hörnesite	Mg₃(AsO₄)₂ · 8H₂O
As	ⓘ Lautite	CuAsS
As	ⓘ Löllingite	FeAs₂
As	ⓘ Mcnearite	NaCa₅(AsO₄)(HAsO₄)₄ · 4H₂O
As	ⓘ Mimetite	Pb₅(AsO₄)₃Cl
As	ⓘ Nickelskutterudite	NiAs₃
As	ⓘ Nickeline	NiAs
As	ⓘ Orpiment	As₂S₃
As	ⓘ Pararammelsbergite	NiAs₂
As	ⓘ Pearceite	[Ag₆As₂S₇][Ag₉CuS₄]
As	ⓘ Pharmacolite	Ca(HAsO₄) · 2H₂O
As	ⓘ Phaunouxite	Ca₃(AsO₄)₂ · 11H₂O
As	ⓘ Picropharmacolite	Ca₄Mg(AsO₄)₂(HAsO₄)₂ · 11H₂O
As	ⓘ Proustite	Ag₃AsS₃
As	ⓘ Rammelsbergite	NiAs₂
As	ⓘ Rauenthalite	Ca₃(AsO₄)₂ · 10H₂O
As	ⓘ Realgar	As₄S₄
As	ⓘ Rösslerite	Mg(HAsO₄) · 7H₂O
As	ⓘ Safflorite	(Co,Ni,Fe)As₂
As	ⓘ Sainfeldite	Ca₅(AsO₄)₂(AsO₃OH)₂ · 4H₂O
As	ⓘ Scorodite	Fe³⁺AsO₄ · 2H₂O
As	ⓘ Skutterudite	CoAs₃
As	ⓘ Tennantite Subgroup	Cu₆(Cu₄C₂²⁺)As₄S₁₂S
As	ⓘ Weilite	Ca(HAsO₄)
As	ⓘ Xanthoconite	Ag₃AsS₃
As	ⓘ Giftgrubeite	CaMn₂Ca₂(AsO₄)₂(AsO₃OH)₂ · 4H₂O
Ag	Silver
Ag	ⓘ Acanthite	Ag₂S
Ag	ⓘ Argentopyrite	AgFe₂S₃
Ag	ⓘ Aramayoite	Ag₃Sb₂(Bi,Sb)S₆
Ag	ⓘ Berryite	Cu₃Ag₂Pb₃Bi₇S₁₆
Ag	ⓘ Chlorargyrite	AgCl
Ag	ⓘ Dervillite	Ag₂AsS₂
Ag	ⓘ Dyscrasite	Ag₃Sb
Ag	ⓘ Matildite	AgBiS₂
Ag	ⓘ Miargyrite	AgSbS₂
Ag	ⓘ Pavonite	AgBi₃S₅
Ag	ⓘ Pearceite	[Ag₆As₂S₇][Ag₉CuS₄]
Ag	ⓘ Polybasite	[Ag₆Sb₂S₇][Ag₉CuS₄]
Ag	ⓘ Proustite	Ag₃AsS₃
Ag	ⓘ Pyrargyrite	Ag₃SbS₃
Ag	ⓘ Native Silver	Ag
Ag	ⓘ Xanthoconite	Ag₃AsS₃
Ag	ⓘ Baumstarkite	Ag₃Sb₃S₆
Sb	Antimony
Sb	ⓘ Aramayoite	Ag₃Sb₂(Bi,Sb)S₆
Sb	ⓘ Bournonite	PbCuSbS₃
Sb	ⓘ Dyscrasite	Ag₃Sb
Sb	ⓘ Kobellite	Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉
Sb	ⓘ Miargyrite	AgSbS₂
Sb	ⓘ Polybasite	[Ag₆Sb₂S₇][Ag₉CuS₄]
Sb	ⓘ Pyrargyrite	Ag₃SbS₃
Sb	ⓘ Semseyite	Pb₉Sb₈S₂₁
Sb	ⓘ Tetrahedrite Subgroup	Cu₆(Cu₄C₂²⁺)Sb₄S₁₂S
Sb	ⓘ Baumstarkite	Ag₃Sb₃S₆
Pb	Lead
Pb	ⓘ Aikinite	CuPbBiS₃
Pb	ⓘ Berryite	Cu₃Ag₂Pb₃Bi₇S₁₆
Pb	ⓘ Bournonite	PbCuSbS₃
Pb	ⓘ Cosalite	Pb₂Bi₂S₅
Pb	ⓘ Galena	PbS
Pb	ⓘ Kobellite	Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉
Pb	ⓘ Mimetite	Pb₅(AsO₄)₃Cl
Pb	ⓘ Pyromorphite	Pb₅(PO₄)₃Cl
Pb	ⓘ Semseyite	Pb₉Sb₈S₂₁
Bi	Bismuth
Bi	ⓘ Aikinite	CuPbBiS₃
Bi	ⓘ Aramayoite	Ag₃Sb₂(Bi,Sb)S₆
Bi	ⓘ Berryite	Cu₃Ag₂Pb₃Bi₇S₁₆
Bi	ⓘ Native Bismuth	Bi
Bi	ⓘ Bismuthinite	Bi₂S₃
Bi	ⓘ Cosalite	Pb₂Bi₂S₅
Bi	ⓘ Emplectite	CuBiS₂
Bi	ⓘ Kobellite	Pb₂₂Cu₄(Bi,Sb)₃₀S₆₉
Bi	ⓘ Matildite	AgBiS₂
Bi	ⓘ Pavonite	AgBi₃S₅
Bi	ⓘ Wittichenite	Cu₃BiS₃

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate

Moldanubian BeltOrogenic Belt

EuropeContinent

France

⭔AlsaceRegion
Grand Est
- Vosges
  - Vosges Volcanic FieldVolcanic Field

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