Lammerite

lammerite

tolbachite

fedotovite

klyuchevskite

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Formula: Cu3(AsO4)2
Anhydrous normal arsenate
Crystal System: Monoclinic
Specific gravity: measured 4.9 - 5.18, calculated 5.236
Hardness: 3½ to 4
Streak: Pale green
Colour: Dark green
Environments

Hydrothermal environments
Fumeroles

Localities

At the type locality, the Laurani mine, Laurani District, Aroma Province, La Paz, Bolivia, lammerite was found on an old mineral specimen as dark green spheroidal aggregates ~0.5 cm in diameter on corroded quartz rock associated with olivenite (Mindat).

At the Tsumeb Mine, Tsumeb, Oshikoto Region, Namibia, lammerite occurs in an oxidised zone in a dolostone-hosted hydrothermal polymetallic ore deposit. Associated minerals include chalcanthite, anhydrite and leightonite (HOM).

At the Tolbachik volcano, Kamchatka Krai, Russia, lammerite occurs in fumeroles. Associated minerals include euchlorine, melanothallite, dolerophanite, chalcocyanite, leningradite, tolbachite, anglesite, alarsite, fedotovite, klyuchevskite, nabokoite, atlasovite, langbeinite, hematite and tenorite (HOM).
All Tolbachik arsenates crystallised at temperatures greater than 450°C (the major assumed temperature interval is 500 to 750°C), under atmospheric pressure. They were precipitated directly from the gas phase as volcanic sublimates, or were formed as a result of gas–rock interaction in fumaroles, where the host basalt was the source of the less volatile elements aluminium, titanium, magnesium and calcium (EJM 30.305-322).

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