Dossi di Franscia, Franscia, Lanzada, Sondrio Province, Lombardy, Italyi
Regional Level Types | |
---|---|
Dossi di Franscia | Group of Hills |
Franscia | Village |
Lanzada | Municipality |
Sondrio Province | Province |
Lombardy | Region |
Italy | - not defined - |
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Latitude & Longitude (WGS84):
46° 17' 17'' North , 9° 54' 15'' East
Latitude & Longitude (decimal):
Area:
1.0 km2
Type:
Group of Hills
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Lanzada | 1,365 (2014) | 3.4km |
Vassalini | 247 (2014) | 4.0km |
Caspoggio | 1,375 (2014) | 4.2km |
Santa Elisabetta | 123 (2014) | 4.5km |
Chiesa in Valmalenco | 2,203 (2014) | 4.8km |
Mindat Locality ID:
2084
Long-form identifier:
mindat:1:2:2084:1
GUID (UUID V4):
c6e3da6a-d227-4dd6-9732-e1d50439d3de
Other/historical names associated with this locality:
Franscia Mine; Franscia Mines; Franscia Quarries
Name(s) in local language(s):
Dossi di Franscia (Miniera di Franscia; Miniere di Franscia; Cave di Franscia), Campo Franscia (Franscia), Lanzada, Val Lanterna, Valmalenco (Val Malenco), Valtellina, Sondrio, Lombardia, Italia
At Dossi di Franscia, a group of hillocks to the SSW of Campo Franscia (Franscia) village, the various mineral sites can be grouped into:
- ancient asbestos mines and prospecting works;
- serpentinite quarries;
- outcrops of mineralised veins and lenses in the country-rock.
Minerals occur in different formation environments inside serpentinite:
- asbestos-andradite clefts;
- carbonate-rich fissures;
- titanian hydroxylclinohumite-forsterite-calcite veins;
- rodingite dykes;
- carbonate veins (hydrothermalites) with Ti-Ni-Cu minerals;
- chromitite lenses and veins.
Asbestos-andradite clefts are the source of remarkable specimens of demantoid. For demantoid and fibrous chrysotile, the best finds are recorded from the ancient mines, locally named “Trona Granda”, located in front of the building of Ristoro di Franscia and below the present Mauri serpentinite quarry (now they are collapsed) (Sigismund, 1948; Gramaccioli, 1962 and other authors). Various other mines, quarries, prospecting works, and outcrops sporadically yielded good specimens of demantoid and fibrous chrysotile, such as:
- the serpentinite quarries (Mauri and Gerosa quarries) located in the proximity of the building of Ristoro di Franscia, below the spurs of Ciudé or Piodé (an elevation at the east foot of Motta Mt.);
- some old galleries in the little valley beneath the building of Ristoro di Franscia;
- the hillock overhanging the building of Ristoro di Franscia. Here, demantoid typically forms lenticular or spheroidal crystal nodules, attaining various centimetres in diameter, named “asbestos seed” (“semenza d’amianto”) by the miners/quarrymen.
Hydrated magnesium carbonates are sporadically found inside serpentinite fissures. Artinite was described as a new mineral species on specimens, consisting of white radiating veinlets, collected by Pietro Sigismund in the summer of 1902 at the old municipal asbestos mine, located behind the chapel of Dossi di Franscia (Brugnatelli, 1902 and 1906). A large fissure lined with artinite, as spherules of acicular crystals up to 2 cm in diameter, in association with hydromagnesite and probably coalingite, was found during the winter of 1987-88 at the Mauri serpentinite quarry. The first find of nesquehonite was recorded in 1921 from the “Trona Granda” asbestos mines (Artini, 1921).
Rodingite dykes crop out a few tens of meters from Ristoro di Franscia. Typical minerals are:
- colourless to white small crystals of diopside;
- colourless, pinkish or yellow rhombododecahedral crystals of grossular;
- green and yellow prismatic crystals of vesuvianite with red-brown terminations.
Associated minerals include clinochlore, calcite, chalcocite, bornite, and malachite.
White veins of fibrous pectolite, in association with creamy calcite, embedded in a chlorite-rich facies were found at the beginning of the 1960s to the west of Ristoro di Franscia. Acicular pectolite crystals up to 2 cm are known from the cavities in the compact mineral.
Magnetite, dolomite, pecoraite, and heazlewoodite in carbonate veins (hydrothermalites) have been found in the dump of an abandoned mine near Ristoro di Franscia (Bedognè et al., 1993).
Finds of copper minerals (native copper, bornite, chalcocite, and cuprite) and other species (rutile, quartz, apatite, brucite, etc.) were reported by Sigismund (1947).
Chromitite lenses and veins at Dossi di Franscia are known for a long time. A chromitite lens was reported from the Ciatùn asbestos mine, currently no longer identifiable on the territory, but whose location is probably in the area of the present Mauri serpentinite quarry. It was the source of bright emerald-green crystals of “uvarovite” (actually chromian andradite) in association with violet chromian clinochlore, asbestos, and probable sepiolite (Sigismund, 1948; Gramaccioli, 1962). Reevesite, zaratite, theophrastite, brucite, calcite, and prehnite have been found on the fractures of chromitite blocks from the dumps in the neighbourhood of Ristoro di Franscia. Chromitite lenses have also been found at the Mauri and Gerosa serpentinite quarries. A chromitite vein crops out in one of the abandoned adits to the southeast of Ristoro di Franscia.
NOTES
Artinite: Dossi di Franscia is the type locality for this mineral species, discovered by Pietro Sigismund (1874-1962), mineral collector and pioneer mineral seeker in Valtellina, in the summer of 1902 at the old municipal asbestos mine, located behind the chapel of Dossi di Franscia (Brugnatelli, 1902 and 1906). However, six years earlier, Luigi Brugnatelli already studied an identical hydrated magnesium carbonate (Brugnatelli, 1897 and 1899) which he personally collected in Valbrutta (Val Brutta). From the chemical analysis he deduced the formula MgCO3•Mg(OH)2•3H2O, but, due to the scarcity of the analysed material (0.171 g including impurities), Brugnatelli thought it was prudent to wait for a new analysis before recognising the mineral as a new species. The new analysis, that he performed on the abundant Sigismund's material forwarded through Ettore Artini, confirmed the two finds to be identical.
"Uvarovite": emerald-green crystals in chromitite fissures, traditionally considered to be "uvarovite" (Sigismund, 1948; Gramaccioli, 1962; De Michele, 1972, and other authors), are actually chromian andradite with a content in Cr2O3 varying inside the crystals from 9.6% in the core to 0.8% at the rim (Bedognè et al., 1993; Sciesa, 1993).
“Ti-bearing clinohumite; titanclinohumite”: according to the analyses performed, this mineral in the Malenco valley serpentinite is practically fluorine-free (Trommsdorff and Evans, 1980). Therefore, after the institution of the new species hydroxylclinohumite in 1999, all records of “titanclinohumite” in the antecedent literature and all specimens preserved in public and private collections consequently labelled are now Ti-bearing hydroxylclinohumite (Bedognè et al., 2006).
Mauri quarry: one of the two active serpentinite quarries at Dossi di Franscia is operated by the company Marmi Mauri S.r.l. As the same company operates three serpentinite quarries in the municipal territory of Lanzada (at Le Prese, Valbrutta, and Dossi di Franscia respectively), some confusion can arise about the exact provenance of specimens simply labelled as from “Mauri quarry, Lanzada”. Nevertheless, the name Mauri quarry has been generally used among the mineral collectors to indicate the one located at Le Prese (http://www.mindat.org/loc-233994.html), where vesuvianite-rich rodingite dykes have been evidenced.
Provided geographical coordinates refer to the still-active "Dossi di Franscia" Quarry. The whole collecting area, as here described, encompasses several sub-localities in a radius of about 1 km.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
44 valid minerals. 1 (TL) - type locality of valid minerals. 2 erroneous literature entries.
Detailed Mineral List:
ⓘ Andradite Formula: Ca3Fe3+2(SiO4)3 |
ⓘ Andradite var. Demantoid Formula: Ca3Fe3+2(SiO4)3 |
ⓘ Antigorite Formula: Mg3(Si2O5)(OH)4 |
ⓘ 'Apatite' Formula: Ca5(PO4)3(Cl/F/OH) |
ⓘ Aragonite Formula: CaCO3 |
ⓘ Artinite (TL) Formula: Mg2(CO3)(OH)2 · 3H2O Type Locality: References: |
ⓘ 'Asbestos' |
ⓘ Formula: Bi2S3 Description: No references in literature. |
ⓘ Bornite Formula: Cu5FeS4 |
ⓘ Brucite Formula: Mg(OH)2 |
ⓘ Calcite Formula: CaCO3 |
ⓘ Chalcocite Formula: Cu2S |
ⓘ Chalcopyrite Formula: CuFeS2 |
ⓘ 'Chlorite Group' |
ⓘ Chromite Formula: Fe2+Cr3+2O4 |
ⓘ Chrysotile Formula: Mg3(Si2O5)(OH)4 |
ⓘ Clinochlore Formula: Mg5Al(AlSi3O10)(OH)8 |
ⓘ Clinochlore var. Chromium-bearing Clinochlore Formula: Mg5(Al,Cr)2Si3O10(OH)8 |
ⓘ Clinohumite Formula: Mg9(SiO4)4F2 |
ⓘ Coalingite ? Formula: Mg10Fe3+2(OH)24[CO3] · 2H2O |
ⓘ Copper Formula: Cu |
ⓘ Cuprite Formula: Cu2O |
ⓘ Diopside Formula: CaMgSi2O6 |
ⓘ Dolomite Formula: CaMg(CO3)2 |
ⓘ Epsomite ? Formula: MgSO4 · 7H2O |
ⓘ Forsterite Formula: Mg2SiO4 |
ⓘ Grossular Formula: Ca3Al2(SiO4)3 |
ⓘ Heazlewoodite Formula: Ni3S2 |
ⓘ Hydromagnesite Formula: Mg5(CO3)4(OH)2 · 4H2O |
ⓘ Hydroxylclinohumite var. Titanclinohumite Formula: (Mg,Ti)9(SiO4)4(OH,F)2 |
ⓘ Magnesite Formula: MgCO3 |
ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
ⓘ Morenosite Formula: NiSO4 · 7H2O Description: The supposition that the morenosite find simply reported in Palache et al. (1951) as from Val Malenco could be referred to Dossi di Franscia is incorrect. In fact, analysis #4 in the annexed table of selected analytical data gives the reference to Cavinato's publication (1936), in which morenosite from Primolo (Chiesa in Valmalenco) was described. |
ⓘ Nesquehonite Formula: MgCO3 · 3H2O References: |
ⓘ Pecoraite ? Formula: Ni3(Si2O5)(OH)4 |
ⓘ Pectolite Formula: NaCa2Si3O8(OH) |
ⓘ Pentlandite Formula: (NixFey)Σ9S8 |
ⓘ Perovskite Formula: CaTiO3 |
ⓘ Prehnite Formula: Ca2Al2Si3O10(OH)2 |
ⓘ Pyrite Formula: FeS2 |
ⓘ Quartz Formula: SiO2 |
ⓘ Reevesite Formula: Ni6Fe3+2(OH)16(CO3) · 4H2O |
ⓘ Rutile Formula: TiO2 |
ⓘ Sepiolite Formula: Mg4(Si6O15)(OH)2 · 6H2O |
ⓘ Sphalerite Formula: ZnS |
ⓘ Talc Formula: Mg3Si4O10(OH)2 |
ⓘ Theophrastite Formula: Ni(OH)2 |
ⓘ Tremolite Formula: ◻Ca2Mg5(Si8O22)(OH)2 |
ⓘ Formula: Ca3Cr2(SiO4)3 Description: Emerald-green garnet crystals in chromitite fissures, traditionally considered “uvarovite” (Sigismund, 1948; Gramaccioli, 1962; De Michele, 1972, and other authors), are actually Cr-bearing andradite with a content in Cr2O3 varying inside the crystals from 9.6% in the core to 0.8% at the rim (Bedognè et al., 1993; Sciesa, 1993). References: |
ⓘ Vesuvianite Formula: Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
ⓘ Zaratite Formula: Ni3(CO3)(OH)4 · 4H2O ? |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Copper | 1.AA.05 | Cu |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Chalcocite | 2.BA.05 | Cu2S |
ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
ⓘ | Heazlewoodite | 2.BB.05 | Ni3S2 |
ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
ⓘ | Sphalerite | 2.CB.05a | ZnS |
ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
ⓘ | Bismuthinite ? | 2.DB.05 | Bi2S3 |
ⓘ | Pyrite | 2.EB.05a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Cuprite | 4.AA.10 | Cu2O |
ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
ⓘ | Perovskite | 4.CC.30 | CaTiO3 |
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | Rutile | 4.DB.05 | TiO2 |
ⓘ | Brucite | 4.FE.05 | Mg(OH)2 |
ⓘ | Theophrastite | 4.FE.05 | Ni(OH)2 |
Group 5 - Nitrates and Carbonates | |||
ⓘ | Magnesite | 5.AB.05 | MgCO3 |
ⓘ | Calcite | 5.AB.05 | CaCO3 |
ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
ⓘ | Aragonite | 5.AB.15 | CaCO3 |
ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
ⓘ | Nesquehonite | 5.CA.05 | MgCO3 · 3H2O |
ⓘ | Hydromagnesite | 5.DA.05 | Mg5(CO3)4(OH)2 · 4H2O |
ⓘ | Artinite (TL) | 5.DA.10 | Mg2(CO3)(OH)2 · 3H2O |
ⓘ | Zaratite | 5.DA.15 | Ni3(CO3)(OH)4 · 4H2O ? |
ⓘ | Reevesite | 5.DA.50 | Ni6Fe3+2(OH)16(CO3) · 4H2O |
ⓘ | Coalingite ? | 5.DA.55 | Mg10Fe3+2(OH)24[CO3] · 2H2O |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
ⓘ | Epsomite ? | 7.CB.40 | MgSO4 · 7H2O |
ⓘ | Morenosite | 7.CB.40 | NiSO4 · 7H2O |
Group 9 - Silicates | |||
ⓘ | Chrysotile | 9.. | Mg3(Si2O5)(OH)4 |
ⓘ | Forsterite | 9.AC.05 | Mg2SiO4 |
ⓘ | Uvarovite ? | 9.AD.25 | Ca3Cr2(SiO4)3 |
ⓘ | Andradite | 9.AD.25 | Ca3Fe3+2(SiO4)3 |
ⓘ | var. Demantoid | 9.AD.25 | Ca3Fe3+2(SiO4)3 |
ⓘ | Grossular | 9.AD.25 | Ca3Al2(SiO4)3 |
ⓘ | Clinohumite | 9.AF.55 | Mg9(SiO4)4F2 |
ⓘ | Hydroxylclinohumite var. Titanclinohumite | 9.AF.55 | (Mg,Ti)9(SiO4)4(OH,F)2 |
ⓘ | Vesuvianite | 9.BG.35 | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
ⓘ | Tremolite | 9.DE.10 | ◻Ca2Mg5(Si8O22)(OH)2 |
ⓘ | Pectolite | 9.DG.05 | NaCa2Si3O8(OH) |
ⓘ | Prehnite | 9.DP.20 | Ca2Al2Si3O10(OH)2 |
ⓘ | Talc | 9.EC.05 | Mg3Si4O10(OH)2 |
ⓘ | Clinochlore | 9.EC.55 | Mg5Al(AlSi3O10)(OH)8 |
ⓘ | var. Chromium-bearing Clinochlore | 9.EC.55 | Mg5(Al,Cr)2Si3O10(OH)8 |
ⓘ | Pecoraite ? | 9.ED.15 | Ni3(Si2O5)(OH)4 |
ⓘ | Antigorite | 9.ED.15 | Mg3(Si2O5)(OH)4 |
ⓘ | Sepiolite | 9.EE.25 | Mg4(Si6O15)(OH)2 · 6H2O |
Unclassified | |||
ⓘ | 'Chlorite Group' | - | |
ⓘ | 'Asbestos' | - | |
ⓘ | 'Apatite' | - | Ca5(PO4)3(Cl/F/OH) |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
H | ⓘ Artinite | Mg2(CO3)(OH)2 · 3H2O |
H | ⓘ Brucite | Mg(OH)2 |
H | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
H | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
H | ⓘ Coalingite | Mg10Fe23+(OH)24[CO3] · 2H2O |
H | ⓘ Epsomite | MgSO4 · 7H2O |
H | ⓘ Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O |
H | ⓘ Clinochlore var. Chromium-bearing Clinochlore | Mg5(Al,Cr)2Si3O10(OH)8 |
H | ⓘ Malachite | Cu2(CO3)(OH)2 |
H | ⓘ Morenosite | NiSO4 · 7H2O |
H | ⓘ Nesquehonite | MgCO3 · 3H2O |
H | ⓘ Pecoraite | Ni3(Si2O5)(OH)4 |
H | ⓘ Pectolite | NaCa2Si3O8(OH) |
H | ⓘ Prehnite | Ca2Al2Si3O10(OH)2 |
H | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
H | ⓘ Sepiolite | Mg4(Si6O15)(OH)2 · 6H2O |
H | ⓘ Talc | Mg3Si4O10(OH)2 |
H | ⓘ Theophrastite | Ni(OH)2 |
H | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
H | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
H | ⓘ Zaratite | Ni3(CO3)(OH)4 · 4H2O ? |
H | ⓘ Hydroxylclinohumite var. Titanclinohumite | (Mg,Ti)9(SiO4)4(OH,F)2 |
H | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
C | Carbon | |
C | ⓘ Aragonite | CaCO3 |
C | ⓘ Artinite | Mg2(CO3)(OH)2 · 3H2O |
C | ⓘ Calcite | CaCO3 |
C | ⓘ Coalingite | Mg10Fe23+(OH)24[CO3] · 2H2O |
C | ⓘ Dolomite | CaMg(CO3)2 |
C | ⓘ Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O |
C | ⓘ Magnesite | MgCO3 |
C | ⓘ Malachite | Cu2(CO3)(OH)2 |
C | ⓘ Nesquehonite | MgCO3 · 3H2O |
C | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
C | ⓘ Zaratite | Ni3(CO3)(OH)4 · 4H2O ? |
O | Oxygen | |
O | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
O | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
O | ⓘ Aragonite | CaCO3 |
O | ⓘ Artinite | Mg2(CO3)(OH)2 · 3H2O |
O | ⓘ Brucite | Mg(OH)2 |
O | ⓘ Calcite | CaCO3 |
O | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
O | ⓘ Chromite | Fe2+Cr23+O4 |
O | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
O | ⓘ Clinohumite | Mg9(SiO4)4F2 |
O | ⓘ Coalingite | Mg10Fe23+(OH)24[CO3] · 2H2O |
O | ⓘ Cuprite | Cu2O |
O | ⓘ Andradite var. Demantoid | Ca3Fe23+(SiO4)3 |
O | ⓘ Diopside | CaMgSi2O6 |
O | ⓘ Dolomite | CaMg(CO3)2 |
O | ⓘ Epsomite | MgSO4 · 7H2O |
O | ⓘ Forsterite | Mg2SiO4 |
O | ⓘ Grossular | Ca3Al2(SiO4)3 |
O | ⓘ Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O |
O | ⓘ Clinochlore var. Chromium-bearing Clinochlore | Mg5(Al,Cr)2Si3O10(OH)8 |
O | ⓘ Magnesite | MgCO3 |
O | ⓘ Magnetite | Fe2+Fe23+O4 |
O | ⓘ Malachite | Cu2(CO3)(OH)2 |
O | ⓘ Morenosite | NiSO4 · 7H2O |
O | ⓘ Nesquehonite | MgCO3 · 3H2O |
O | ⓘ Pecoraite | Ni3(Si2O5)(OH)4 |
O | ⓘ Pectolite | NaCa2Si3O8(OH) |
O | ⓘ Perovskite | CaTiO3 |
O | ⓘ Prehnite | Ca2Al2Si3O10(OH)2 |
O | ⓘ Quartz | SiO2 |
O | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
O | ⓘ Rutile | TiO2 |
O | ⓘ Sepiolite | Mg4(Si6O15)(OH)2 · 6H2O |
O | ⓘ Talc | Mg3Si4O10(OH)2 |
O | ⓘ Theophrastite | Ni(OH)2 |
O | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
O | ⓘ Uvarovite | Ca3Cr2(SiO4)3 |
O | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
O | ⓘ Zaratite | Ni3(CO3)(OH)4 · 4H2O ? |
O | ⓘ Hydroxylclinohumite var. Titanclinohumite | (Mg,Ti)9(SiO4)4(OH,F)2 |
O | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
F | Fluorine | |
F | ⓘ Clinohumite | Mg9(SiO4)4F2 |
F | ⓘ Hydroxylclinohumite var. Titanclinohumite | (Mg,Ti)9(SiO4)4(OH,F)2 |
F | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
Na | Sodium | |
Na | ⓘ Pectolite | NaCa2Si3O8(OH) |
Mg | Magnesium | |
Mg | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
Mg | ⓘ Artinite | Mg2(CO3)(OH)2 · 3H2O |
Mg | ⓘ Brucite | Mg(OH)2 |
Mg | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
Mg | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
Mg | ⓘ Clinohumite | Mg9(SiO4)4F2 |
Mg | ⓘ Coalingite | Mg10Fe23+(OH)24[CO3] · 2H2O |
Mg | ⓘ Diopside | CaMgSi2O6 |
Mg | ⓘ Dolomite | CaMg(CO3)2 |
Mg | ⓘ Epsomite | MgSO4 · 7H2O |
Mg | ⓘ Forsterite | Mg2SiO4 |
Mg | ⓘ Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O |
Mg | ⓘ Clinochlore var. Chromium-bearing Clinochlore | Mg5(Al,Cr)2Si3O10(OH)8 |
Mg | ⓘ Magnesite | MgCO3 |
Mg | ⓘ Nesquehonite | MgCO3 · 3H2O |
Mg | ⓘ Sepiolite | Mg4(Si6O15)(OH)2 · 6H2O |
Mg | ⓘ Talc | Mg3Si4O10(OH)2 |
Mg | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
Mg | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
Mg | ⓘ Hydroxylclinohumite var. Titanclinohumite | (Mg,Ti)9(SiO4)4(OH,F)2 |
Al | Aluminium | |
Al | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
Al | ⓘ Grossular | Ca3Al2(SiO4)3 |
Al | ⓘ Clinochlore var. Chromium-bearing Clinochlore | Mg5(Al,Cr)2Si3O10(OH)8 |
Al | ⓘ Prehnite | Ca2Al2Si3O10(OH)2 |
Al | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
Si | Silicon | |
Si | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
Si | ⓘ Antigorite | Mg3(Si2O5)(OH)4 |
Si | ⓘ Chrysotile | Mg3(Si2O5)(OH)4 |
Si | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
Si | ⓘ Clinohumite | Mg9(SiO4)4F2 |
Si | ⓘ Andradite var. Demantoid | Ca3Fe23+(SiO4)3 |
Si | ⓘ Diopside | CaMgSi2O6 |
Si | ⓘ Forsterite | Mg2SiO4 |
Si | ⓘ Grossular | Ca3Al2(SiO4)3 |
Si | ⓘ Clinochlore var. Chromium-bearing Clinochlore | Mg5(Al,Cr)2Si3O10(OH)8 |
Si | ⓘ Pecoraite | Ni3(Si2O5)(OH)4 |
Si | ⓘ Pectolite | NaCa2Si3O8(OH) |
Si | ⓘ Prehnite | Ca2Al2Si3O10(OH)2 |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Sepiolite | Mg4(Si6O15)(OH)2 · 6H2O |
Si | ⓘ Talc | Mg3Si4O10(OH)2 |
Si | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
Si | ⓘ Uvarovite | Ca3Cr2(SiO4)3 |
Si | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
Si | ⓘ Hydroxylclinohumite var. Titanclinohumite | (Mg,Ti)9(SiO4)4(OH,F)2 |
P | Phosphorus | |
P | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
S | Sulfur | |
S | ⓘ Bismuthinite | Bi2S3 |
S | ⓘ Bornite | Cu5FeS4 |
S | ⓘ Chalcopyrite | CuFeS2 |
S | ⓘ Chalcocite | Cu2S |
S | ⓘ Epsomite | MgSO4 · 7H2O |
S | ⓘ Heazlewoodite | Ni3S2 |
S | ⓘ Morenosite | NiSO4 · 7H2O |
S | ⓘ Pentlandite | (NixFey)Σ9S8 |
S | ⓘ Pyrite | FeS2 |
S | ⓘ Sphalerite | ZnS |
Cl | Chlorine | |
Cl | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
Ca | Calcium | |
Ca | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
Ca | ⓘ Aragonite | CaCO3 |
Ca | ⓘ Calcite | CaCO3 |
Ca | ⓘ Andradite var. Demantoid | Ca3Fe23+(SiO4)3 |
Ca | ⓘ Diopside | CaMgSi2O6 |
Ca | ⓘ Dolomite | CaMg(CO3)2 |
Ca | ⓘ Grossular | Ca3Al2(SiO4)3 |
Ca | ⓘ Pectolite | NaCa2Si3O8(OH) |
Ca | ⓘ Perovskite | CaTiO3 |
Ca | ⓘ Prehnite | Ca2Al2Si3O10(OH)2 |
Ca | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
Ca | ⓘ Uvarovite | Ca3Cr2(SiO4)3 |
Ca | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
Ca | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
Ti | Titanium | |
Ti | ⓘ Perovskite | CaTiO3 |
Ti | ⓘ Rutile | TiO2 |
Ti | ⓘ Hydroxylclinohumite var. Titanclinohumite | (Mg,Ti)9(SiO4)4(OH,F)2 |
Cr | Chromium | |
Cr | ⓘ Chromite | Fe2+Cr23+O4 |
Cr | ⓘ Clinochlore var. Chromium-bearing Clinochlore | Mg5(Al,Cr)2Si3O10(OH)8 |
Cr | ⓘ Uvarovite | Ca3Cr2(SiO4)3 |
Fe | Iron | |
Fe | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
Fe | ⓘ Bornite | Cu5FeS4 |
Fe | ⓘ Chalcopyrite | CuFeS2 |
Fe | ⓘ Chromite | Fe2+Cr23+O4 |
Fe | ⓘ Coalingite | Mg10Fe23+(OH)24[CO3] · 2H2O |
Fe | ⓘ Andradite var. Demantoid | Ca3Fe23+(SiO4)3 |
Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
Fe | ⓘ Pentlandite | (NixFey)Σ9S8 |
Fe | ⓘ Pyrite | FeS2 |
Fe | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
Fe | ⓘ Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 |
Ni | Nickel | |
Ni | ⓘ Heazlewoodite | Ni3S2 |
Ni | ⓘ Morenosite | NiSO4 · 7H2O |
Ni | ⓘ Pecoraite | Ni3(Si2O5)(OH)4 |
Ni | ⓘ Pentlandite | (NixFey)Σ9S8 |
Ni | ⓘ Reevesite | Ni6Fe23+(OH)16(CO3) · 4H2O |
Ni | ⓘ Theophrastite | Ni(OH)2 |
Ni | ⓘ Zaratite | Ni3(CO3)(OH)4 · 4H2O ? |
Cu | Copper | |
Cu | ⓘ Bornite | Cu5FeS4 |
Cu | ⓘ Chalcopyrite | CuFeS2 |
Cu | ⓘ Chalcocite | Cu2S |
Cu | ⓘ Cuprite | Cu2O |
Cu | ⓘ Copper | Cu |
Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
Zn | Zinc | |
Zn | ⓘ Sphalerite | ZnS |
Bi | Bismuth | |
Bi | ⓘ Bismuthinite | Bi2S3 |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
EuropeContinent
- The AlpsMountain Range
Italy
- Lombardy
- Sondrio Province
- Malenco ValleyValley
- Lanterna ValleyValley
- ValtellinaValley
- Malenco ValleyValley
- Sondrio Province
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