Matilde Mine, La Viñuela, Málaga, Andalusia, Spaini
| Regional Level Types | |
|---|---|
| Matilde Mine | Mine (Built Over) |
| La Viñuela | Municipality |
| Málaga | Province |
| Andalusia | Autonomous Community |
| Spain | Country |
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Latitude & Longitude (WGS84):
36° 51' 27'' North , 4° 10' 0'' West
Latitude & Longitude (decimal):
Type:
Mine (Built Over) - last checked 2024
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Viñuela | 1,591 (2018) | 2.4km |
| Benamargosa | 1,547 (2012) | 3.5km |
| Cútar | 638 (2012) | 6.1km |
| Alcaucín | 1,697 (2018) | 6.9km |
| Almáchar | 1,909 (2012) | 7.0km |
Other/historical names associated with this locality:
Victoria Mine; Mina Victoria; "Velez-Malaga"
Name(s) in local language(s):
Mina Matilde ("Velez-Malaga"), la Viñuela, Málaga, España
Antimony mineralization was found during the construction and earthworks of La Viñuela dam, upon an existing ancient mining group. The deposit is located near the west of La Viñuela village, about 17.5 km (road A-356) from the coastline (Torre del Mar). The mineralization was buried by the earthworks dumping from the dam construction.
A previous claim (1887) with the name Victoria Mine was mined by a Scottish company and highlighted in the magazine Andalucia Cientifica (Fondos Sociedad Malagueña de Ciencias at Malaga University Library).
An erroneous name attributed to the same locality is 'Velez-Malaga'.
Antimony mineralization is related to shear zones and a large low-angle reverse fault between grey quartzites and grey-purple andalusite-cordierite-muscovite mica schist with minor brecciated zones. Migmatite sequences close to the site are related to anatexis. The main mineralization fills fractures in quartz veins or even nodules in schistosity of the bedrock, the Alpujarride Complex (see below for literature references). During the construction of the dam and due to the heavy blasting of the existing old mines, large pure masses of antimony were found and collected on site. Once the cut slopes and temporary diversion of the Arroyo Los Montes stream were carried out in 1989, significant veins of antimony were still cropping out on the ground (local workers' confirmation).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Andalusite Formula: Al2(SiO4)O |
| ⓘ Bornite Formula: Cu5FeS4 |
| ⓘ 'Chlorite Group' |
| ⓘ Cordierite Formula: Mg2Al4Si5O18 |
| ⓘ Enargite Formula: Cu3AsS4 |
| ⓘ Graphite Formula: C |
| ⓘ Kermesite Formula: Sb2S2O References: |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Native Antimony Formula: Sb References: |
| ⓘ Quartz Formula: SiO2 References: |
| ⓘ Rutile Formula: TiO2 |
| ⓘ Senarmontite Formula: Sb2O3 |
| ⓘ Stibiconite Formula: Sb3+Sb5+2O6(OH) References: |
| ⓘ Stibnite Formula: Sb2S3 |
| ⓘ Valentinite Formula: Sb2O3 References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Antimony | 1.CA.05 | Sb |
| ⓘ | Graphite | 1.CB.05a | C |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Stibnite | 2.DB.05 | Sb2S3 |
| ⓘ | Kermesite | 2.FD.05 | Sb2S2O |
| ⓘ | Enargite | 2.KA.05 | Cu3AsS4 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Senarmontite | 4.CB.50 | Sb2O3 |
| ⓘ | Valentinite | 4.CB.55 | Sb2O3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| ⓘ | Stibiconite | 4.DH.20 | Sb3+Sb5+2O6(OH) |
| Group 9 - Silicates | |||
| ⓘ | Andalusite | 9.AF.10 | Al2(SiO4)O |
| ⓘ | Cordierite | 9.CJ.10 | Mg2Al4Si5O18 |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| Unclassified | |||
| ⓘ | 'Chlorite Group' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Stibiconite | Sb3+Sb25+O6(OH) |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Graphite | C |
| O | Oxygen | |
| O | ⓘ Andalusite | Al2(SiO4)O |
| O | ⓘ Cordierite | Mg2Al4Si5O18 |
| O | ⓘ Kermesite | Sb2S2O |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Senarmontite | Sb2O3 |
| O | ⓘ Stibiconite | Sb3+Sb25+O6(OH) |
| O | ⓘ Valentinite | Sb2O3 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Mg | Magnesium | |
| Mg | ⓘ Cordierite | Mg2Al4Si5O18 |
| Al | Aluminium | |
| Al | ⓘ Andalusite | Al2(SiO4)O |
| Al | ⓘ Cordierite | Mg2Al4Si5O18 |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Andalusite | Al2(SiO4)O |
| Si | ⓘ Cordierite | Mg2Al4Si5O18 |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Enargite | Cu3AsS4 |
| S | ⓘ Kermesite | Sb2S2O |
| S | ⓘ Stibnite | Sb2S3 |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ti | Titanium | |
| Ti | ⓘ Rutile | TiO2 |
| Fe | Iron | |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Cu | Copper | |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Enargite | Cu3AsS4 |
| As | Arsenic | |
| As | ⓘ Enargite | Cu3AsS4 |
| Sb | Antimony | |
| Sb | ⓘ Native Antimony | Sb |
| Sb | ⓘ Kermesite | Sb2S2O |
| Sb | ⓘ Senarmontite | Sb2O3 |
| Sb | ⓘ Stibiconite | Sb3+Sb25+O6(OH) |
| Sb | ⓘ Stibnite | Sb2S3 |
| Sb | ⓘ Valentinite | Sb2O3 |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
- Betic CordilleraPassive Margin
EuropeContinent
Iberian PeninsulaPeninsula
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Matilde Mine, La Viñuela, Málaga, Andalusia, Spain