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Marabá — Brazilian Source of Green Andalusite

Marabá — Brazilian Source of Green Andalusite

A municipality in Pará state producing the rare olive-green colour of andalusite for the collector market

Localities & originsView in dictionary · 715 words

Marabá is a municipality in the southeastern part of Pará state in northern Brazil, in the Amazon basin, and a documented source of fine green andalusite — the rare colour expression of the species that has made Brazilian andalusite a collector category. The locality is one of relatively few worldwide that has produced commercial quantities of the distinctive yellowish-green to olive-green andalusite that displays the species' characteristic strong pleochroism, with brownish and greenish tints visible along different crystal directions. Marabá andalusite is part of a wider Brazilian gem and mineral output from a region better known historically for its iron, gold, and bauxite mining.

Geological setting

The Marabá region sits within the Carajás mineral province of southeastern Pará, one of the most mineralised geological terrains in South America. The province is best known for the massive iron ore deposits at Carajás and for the gold, copper, manganese, and nickel resources that have driven the region's mining economy. Andalusite occurs in the metamorphic rocks of the broader Brazilian Shield, formed under conditions of regional metamorphism that produce the species in pelitic schists and gneisses. The Marabá deposits are part of this broader metamorphic terrain.

Andalusite is an aluminium silicate (Al2SiO5) that forms one of three polymorphs of the same composition, alongside kyanite and sillimanite. The three minerals form under different temperature and pressure conditions, with andalusite characteristic of relatively low-pressure, moderate-temperature metamorphism. Andalusite is best known among gemmologists for the variety chiastolite, in which carbon inclusions form a cross-pattern visible in cross-sections, but the gem-quality faceted material from Marabá is the transparent, strongly pleochroic form.

The colour and pleochroism

Marabá andalusite typically shows a yellowish-green to olive-green body colour in the principal viewing direction, with strong pleochroism producing brownish and reddish tints along the other crystallographic axes. The pleochroism is one of the species' most distinctive features and is exploited by competent cutters who orient the rough to display two or more colours simultaneously through different facets of the cut stone. A well-cut Brazilian andalusite shows a play of green, brown, and reddish hues that has no clear analogue in other gem species.

The chromophores responsible for the colour include manganese, iron, and titanium in varying combinations, with the specific elemental balance determining the precise hue and pleochroic colours of individual stones. Refractive indices fall in the range 1.629 to 1.648, with birefringence around 0.009 to 0.011, and hardness is 7 to 7.5 on the Mohs scale, sufficient for jewellery use with normal care.

Mining and production

Production from Marabá is modest, typically performed by small-scale operators digging and washing alluvial concentrations in the region's stream beds. The deposits do not support large mechanised operations, and production volumes are small even by the standards of Brazilian gem mining. Fine transparent material in sizes above 5 carats is uncommon, and stones above 10 carats are rare; most commercial production is in the 1 to 5 carat range.

The locality is also known for a range of other minerals, with associated gem minerals including tourmaline and quartz varieties occurring in the same broad metamorphic terrain. The Marabá region's primary economic activity is iron ore mining and other large-scale industrial extraction, with gem production a minor sideline that supplies regional dealers and the international collector market through the established Brazilian gem-trade routes.

In the trade

Brazilian green andalusite from Marabá and other localities reaches the international market through dealers in Belo Horizonte and Teófilo Otoni — the traditional centres of the Brazilian gem trade — and through international gem shows including Tucson and Munich. The material is a niche category, sought by collectors and by jewellery designers seeking unusual coloured stones with strong character. Pricing for fine pleochroic Brazilian andalusite is competitive with other rare collector species in equivalent sizes, with substantial premiums for stones above 5 carats showing strong colour and clean clarity.

Further reading