Beth Mine (Beth-Ghinivert deposit), Troncea Valley, Pragelato, Metropolitan City of Turin, Piedmont, Italyi
| Regional Level Types | |
|---|---|
| Beth Mine (Beth-Ghinivert deposit) | Mine |
| Troncea Valley | Valley |
| Pragelato | Commune |
| Metropolitan City of Turin | Metropolitan City |
| Piedmont | Region |
| Italy | Country |
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Latitude & Longitude (WGS84):
44° 57' 18'' North , 6° 58' 55'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Pragelato-Ruà | 402 (2014) | 7.2km |
| Sestriere | 838 (2012) | 8.2km |
| Colle Sestriere | 646 (2014) | 8.3km |
| Ghigo | 127 (2014) | 9.0km |
| Prali | 266 (2013) | 9.1km |
Name(s) in local language(s):
Miniera del Beth (Giacimento del Beth-Ghinivert), Val Troncea, Pragelato/Massello, Val Chisone, Provincia di Torino, Piemonte, Italia
Copper-iron deposit located in the area of Bric di Mezzogiorno-Colle del Beth-Bric Ghinivert and mined in the period 1860-1910. Some galleries [Vajalet decline or shaft, Bernard decline - see placeholder -, and Beth or Mezzodì gallery] are situated in Troncea Valley (Pragelato, Chisone Valley), others [Monte underground workings; Ghinivert underground workings with the adits named Santa Barbara, San Giacomo, Lantelme and Nicola] are located in Massello Valley (Massello, Germanasca Valley).
Collecting is forbidden in the Troncea Valley sector, because it is part of Val Troncea Natural Park.
The Cu-Fe deposit is characterised by a 0.25–2.5 m thick zone of pyrite-rich stratiform mineralisation associated with metabasites (metagabbros, glaucophanites, and greenschist-facies metabasites) and calcschists (Novarese, 1900; Bouquet & Forette, 1973; Giacometti & Rebay , 2013). Novarese (1900) asserted that the mineralised horizon has a lateral extension of at least 400 m (parallel to dip), a mean thickness of 0.5 m, and is continuous, parallel to the direction of strata, to a depth of at least 80 m. Disseminated sulfides occur in the metabasites at the contact with the stratiform mineralisation. At least two different generations of pyrite have been recorded at Beth; common relicts preserving colloidal textures, which are typical low-temperature hydrothermal features, are overgrown by cubic metamorphic pyrite (Natale, 1966, 1969; Natale & Visetti, 1980). A sedimentary-exhalative origin on the Piedmont Ocean floor has been proposed for the Beth-Ghinivert deposit (Natale & Visetti, 1980).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Aegirine Formula: NaFe3+Si2O6 |
| ⓘ Albite Formula: Na(AlSi3O8) References: Alessandro Cantamessa collectionIdentification: Visual Identification |
| ⓘ Aragonite Formula: CaCO3 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Covellite Formula: CuS |
| ⓘ Deerite Formula: Fe2+6Fe3+3(Si6O17)O3(OH)5 |
| ⓘ Harmotome Formula: Ba2(Si12Al4)O32 · 12H2O |
| ⓘ Hematite Formula: Fe2O3 References: Alessandro Cantamessa collectionIdentification: Visual Identification |
| ⓘ Magnesio-riebeckite Formula: ◻{Na2}{Mg3Fe3+2}(Si8O22)(OH)2 |
| ⓘ Olivenite Formula: Cu2(AsO4)(OH) |
| ⓘ Piemontite Formula: (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| ⓘ Pyrite Formula: FeS2 References: |
| ⓘ Riebeckite Formula: ◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2 |
| ⓘ Stilpnomelane Formula: (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Aragonite | 5.AB.15 | CaCO3 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Olivenite | 8.BB.30 | Cu2(AsO4)(OH) |
| Group 9 - Silicates | |||
| ⓘ | Piemontite | 9.BG.05a | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| ⓘ | Aegirine | 9.DA.25 | NaFe3+Si2O6 |
| ⓘ | Magnesio-riebeckite | 9.DE.25 | ◻{Na2}{Mg3Fe3+2}(Si8O22)(OH)2 |
| ⓘ | Riebeckite | 9.DE.25 | ◻[Na2][Fe2+3Fe3+2]Si8O22(OH)2 |
| ⓘ | Deerite | 9.DH.60 | Fe2+6Fe3+3(Si6O17)O3(OH)5 |
| ⓘ | Stilpnomelane | 9.EG.40 | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| ⓘ | Harmotome | 9.GC.10 | Ba2(Si12Al4)O32 · 12H2O |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Deerite | Fe62+Fe33+(Si6O17)O3(OH)5 |
| H | ⓘ Harmotome | Ba2(Si12Al4)O32 · 12H2O |
| H | ⓘ Magnesio-riebeckite | ◻{Na2}{Mg3Fe23+}(Si8O22)(OH)2 |
| H | ⓘ Olivenite | Cu2(AsO4)(OH) |
| H | ⓘ Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Riebeckite | ◻[Na2][Fe32+Fe23+]Si8O22(OH)2 |
| H | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| C | Carbon | |
| C | ⓘ Aragonite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Aegirine | NaFe3+Si2O6 |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Aragonite | CaCO3 |
| O | ⓘ Deerite | Fe62+Fe33+(Si6O17)O3(OH)5 |
| O | ⓘ Harmotome | Ba2(Si12Al4)O32 · 12H2O |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Magnesio-riebeckite | ◻{Na2}{Mg3Fe23+}(Si8O22)(OH)2 |
| O | ⓘ Olivenite | Cu2(AsO4)(OH) |
| O | ⓘ Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Riebeckite | ◻[Na2][Fe32+Fe23+]Si8O22(OH)2 |
| O | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Na | Sodium | |
| Na | ⓘ Aegirine | NaFe3+Si2O6 |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Magnesio-riebeckite | ◻{Na2}{Mg3Fe23+}(Si8O22)(OH)2 |
| Na | ⓘ Riebeckite | ◻[Na2][Fe32+Fe23+]Si8O22(OH)2 |
| Na | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Mg | Magnesium | |
| Mg | ⓘ Magnesio-riebeckite | ◻{Na2}{Mg3Fe23+}(Si8O22)(OH)2 |
| Mg | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Harmotome | Ba2(Si12Al4)O32 · 12H2O |
| Al | ⓘ Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Si | Silicon | |
| Si | ⓘ Aegirine | NaFe3+Si2O6 |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Deerite | Fe62+Fe33+(Si6O17)O3(OH)5 |
| Si | ⓘ Harmotome | Ba2(Si12Al4)O32 · 12H2O |
| Si | ⓘ Magnesio-riebeckite | ◻{Na2}{Mg3Fe23+}(Si8O22)(OH)2 |
| Si | ⓘ Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Riebeckite | ◻[Na2][Fe32+Fe23+]Si8O22(OH)2 |
| Si | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Covellite | CuS |
| S | ⓘ Pyrite | FeS2 |
| K | Potassium | |
| K | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Ca | Calcium | |
| Ca | ⓘ Aragonite | CaCO3 |
| Ca | ⓘ Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Mn | Manganese | |
| Mn | ⓘ Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) |
| Fe | Iron | |
| Fe | ⓘ Aegirine | NaFe3+Si2O6 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Deerite | Fe62+Fe33+(Si6O17)O3(OH)5 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Magnesio-riebeckite | ◻{Na2}{Mg3Fe23+}(Si8O22)(OH)2 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Riebeckite | ◻[Na2][Fe32+Fe23+]Si8O22(OH)2 |
| Fe | ⓘ Stilpnomelane | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36 · nH2O |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Olivenite | Cu2(AsO4)(OH) |
| As | Arsenic | |
| As | ⓘ Olivenite | Cu2(AsO4)(OH) |
| Ba | Barium | |
| Ba | ⓘ Harmotome | Ba2(Si12Al4)O32 · 12H2O |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
- AlpsAccretionary Complex
EuropeContinent
- The AlpsMountain Range
Italy
- Piedmont
- Metropolitan City of Turin
- Chisone ValleyValley
- Metropolitan City of Turin
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Beth Mine, Troncea Valley, Pragelato, Metropolitan City of Turin, Piedmont, Italy