Aljustrel Mine
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The Mines of Aljustrel () is a
zinc Zinc is a chemical element; it has symbol Zn and atomic number 30. It is a slightly brittle metal at room temperature and has a shiny-greyish appearance when oxidation is removed. It is the first element in group 12 (IIB) of the periodic tabl ...
/
lead Lead () is a chemical element; it has Chemical symbol, symbol Pb (from Latin ) and atomic number 82. It is a Heavy metal (elements), heavy metal that is density, denser than most common materials. Lead is Mohs scale, soft and Ductility, malleabl ...
mine situated in the
civil parish In England, a civil parish is a type of administrative parish used for local government. It is a territorial designation which is the lowest tier of local government. Civil parishes can trace their origin to the ancient system of parishes, w ...
of Aljustrel e Rio de Moinhos, in the
municipality A municipality is usually a single administrative division having municipal corporation, corporate status and powers of self-government or jurisdiction as granted by national and regional laws to which it is subordinate. The term ''municipality' ...
of Aljustrel, in the Portuguese
Alentejo Alentejo ( , , ) is a geographical, historical, and cultural region of south–central and southern Portugal. In Portuguese, its name means "beyond the Tagus" (). Alentejo includes the regions of Alto Alentejo Province, Alto Alentejo and Bai ...
district of Beja. It was classified as a monument in 1982.


History

With more than 80 known deposits, the Iberian Pyrite Belt became an area of intensive mining of sulphide ore since the
Chalcolithic The Chalcolithic ( ) (also called the Copper Age and Eneolithic) was an archaeological period characterized by the increasing use of smelted copper. It followed the Neolithic and preceded the Bronze Age. It occurred at different periods in di ...
era.J.M. Leistel et al (1998), p.3 The Aljustrel camp consists of six separate orebodies (Estação, Feitais, Algares, Moinho, São João and Gavião) that lie on the limbs of four main SWverging folds: the Feitais anticline (towards the northeast), the Central anticline, the São João sincline and the southwestern anticline.Jorge M.R.S. Relvas et al (2011), p.72 The Aljustrel Group structures are truncated and rejected by a major northeast-southwest fault (the Messejana fault). It terminates in the northwest with a hidden by tertiary cover and constitutes the Paleozoic basement where the main two Gavião orebodies occur, with of total massive sulfides. The exploitation of metals in Aljustrel (mining and metallurgy) began at the end of the 3rd millennium BC, with tartessian mines on the hilltop of Nossa Senhora do Castelo, equidistant from iron deposits in Algares and São João do Deserto. Bronze Age excavations were situated in Mangancha, near faults close to São João. At the end of the first century, Mangancha began to be occupied by a Roman settlement, with military garrison, leading to the establishment of a colony at Vipasca, near Algares (today known as Valdoca or Vale da Oca). Mining extended into the 4th century, with production oscillating with crises in the Empire, but was eventually abandoned. Almost all outcroppings and near-surface deposits were exhausted over the centuries and mineral prospecting began in deeper orebodies. Over time, though, pyrite became less important as a raw material in manufacturing of sulfuric acid. Combined with poor base-metal content of these deposits resulted in many mines closing over the last two decades. The mine of ALjustrel only appeared again in the
foral 200px, Foral of Castro Verde - Portugal The ''Carta de Foral'', or simply ''Foral'', was a royal document in Portugal and its former empire, whose purpose was to establish a ''concelho'' (Council) and regulate its administration, borders and priv ...
(''charter'') of 1252, where the Order of Santiago da Espada reserved their right to the profits from the mine. A 16th century regulation, the ''Regulamento Mineiro de Ayres do Quintal'' (''Ayres do Quintal Mining Regulation''), mentioned the mine at Aljustrel. By the middle of the same century, a document from King D. John III, referred to the existence of a pigment produced in the territory, known as ''Azul de Aljustrel'' (''Aljustrel Blue'') that was refined and sold to painters by a regal functionary. An 1848 document attributed the first mining concession in Aljustrel to the Spaniard Sebastião Gargamala, who did little with the claim, and lost the concession. It was later attributed to the Lusitanian Mining Company which, also, only functioned for two years. Two years later, the title was transferred to the Portuguese ''Companhia de Mineração Transtagana'', which began an excavation on a grand scale for the next 15 years, introducing rail transport and mineral treatment in the process. Owing to a series of unfavourable conditions in the international market, the company went bankrupt and the concession was passed to the banking firm Fonseca, Santos & Vianna. The bank became affiliated with a Belgian firm, establishing the ''Société Anonyme Belge des Mines d’Aljustrel'' that reopened the mine in 1973. It continued to operate for the next few years, taking on new partners and assuming various designations. In June 1973, it was taken over by the company Pirites Alentejanas, SARL, with a major stake by national interests (50% by the State, 40% by CUF and a fixed 10% by Mines d’Aljustrel). With the nationalization program implemented by the democratic government in 1975, the State took over 90% of the company's capital assets, with the remaining 10% held by Belgian interests. Yet, in 1977, with discovery of the Neve-Corvo mine (worked by Somincor at the time) containing rich orebodies, lead to renewed exploration due to its economic potential. But, owing to the fall in the price of zinc/lead, beginning in October 2008 the production at the mine was suspended. As a result, the municipal authority pushed to nationalize the concessionaire. With closing of the mine at Aljustrel, the Neves-Corvo mine became the only mine in Portugal.


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* * {{citation , contribution=Structure, stratigraphy and hydrothermal alteration at the Gavião orebodies, Aljustrel: reconstruction of a dismembered ore-forming system at the Iberian Pyrite Belt and implications for exploration , title=11 th SGA Biennial Meeting: Let's Talk Ore Deposits , date=26 September 2011 , location=Antofagasta, Chile , first1=Jorge M.R.S. , last1=Relvas , first2=Fernando J.A.S. , last2=Barriga , first3=João R.S. , last3=Carvalho , first4=Álvaro M.M. , last4=Pinto , first5=João X. , last5=Matos , first6=Carlos JP , last6=Rosa , first7=Zélia , last7=Pereira Mines in Portugal Lead mines Iberian Pyritic Belt Buildings and structures in Beja District Aljustrel Zinc mines in Portugal