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Spodumene

Pyroxene, inosilicate mineral rich in lithium

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The naturally occurring low-temperature form α-spodumene is in the monoclinic system, and the high-temperature β-spodumene crystallizes in the tetragonal system. α-Spodumene converts to β-spodumene at temperatures above 900 °C. Typically crystals are heavily striated along the principal axis. Crystal faces are often etched and pitted with triangular markings.

Discovery and occurrence

Spodumene was first described in 1800 for an occurrence in the type locality in Utö, Södermanland, Sweden. It was discovered by Brazilian naturalist Jose Bonifacio de Andrada e Silva. The name is derived from the Greek spodumenos (σποδούμενος), meaning "burnt to ashes", owing to the opaque ash-grey appearance of material refined for use in industry.

Spodumene occurs in lithium-rich granite pegmatites and aplites. Associated minerals include quartz, albite, petalite, eucryptite, lepidolite, and beryl.

Transparent material has long been used as a gemstone with varieties kunzite and hiddenite noted for their strong pleochroism. Source localities include the Democratic Republic of Congo (DRC), Afghanistan, Australia, Brazil, Madagascar (see mining), Pakistan, Québec in Canada, and North Carolina and California in the U.S.

As of 2018, the DRC was known to have the largest lithium spodumene hard-rock deposit in the world, with mining operations occurring in the central DRC territory of Manono, Tanganyika Province. As of 2021, the Australian company AVZ Minerals was developing the Manono Lithium and Tin project, and had a resource size estimate of 400 million tonnes of high-grade low-impurity ore at 1.65% lithium oxide (Li2O) spodumene hard-rock based on studies and drilling of Roche Dure, one of several pegmatites in the deposit.
Mount Marion contains the world's second-biggest high-grade lithium mineral resources, with an estimated 71 million tonnes (160 billion pounds) of the mineral spodumene under ownership of Mineral Resources and Jiangxi Ganfeng Lithium

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