Dioptase

dioptase

chrysocolla

malachite

wulfenite

Images

Formula: CuSiO3.H2O
Cyclosilicate (ring silicate)
Crystal System: Trigonal
Specific gravity: 3.28 to 3.35 measured, 3.296 calculated
Hardness: 5
Streak: Green
Colour: Emerald green
Solubility: Moderately soluble in hydrochloric acid
Environments:

Hydrothermal environments

Dioptase occurs as a secondary mineral in the oxidised zone of high temperature hydrothermal copper deposits (Webmin, HOM). Associated minerals include chrysocolla, malachite, mimetite, wulfenite, cerussite, hemimorphite, fluorite and quartz (HOM, Mindat).

Localities

At the type locality, the Altyn-Tyube dioptase deposit, Bukhar-Zhyrau, Karaganda Region, Kazakhstan, dioptase occurs as a secondary mineral in the oxidised zones of copper deposits (Mindat).
Altyn-Tyube was mined for copper in the bronze age, and dioptase has been known from there since Roman times, but originally it was thought to be emerald. Well over a thousand years later, towards the end of the eighteenth century, mineralogists began to doubt the identification, and after a bit of argument the name "dioptase" was settled on. The area is remote, poorly mapped and difficult of access, but over the years intrepid mineral collectors have reached it and been rewarded by beautiful specimens.
The limestone at Altyn-Tyube is cut by numerous fissures lined with calcite and dioptase; copper mineralisation is genetically associated with a nearby andesite porphyry intrusion. Hydrothermal alteration deposited quartz, carbonates, baryte and anhydrite in the limestones, and iron-magnesium rich hydrothermal alteration produced a fine-grained epidote-chlorite bearing assemblage in the volcanic rocks.
The primary ore min‌erals at Altyn-Tyube were chalcopyrite, bornite, pyrite and chalcocite, with rare galena and sphalerite. Among the secondary minerals, dioptase is the most pronounced, forming beautiful crystals in cavities in hard, silicified limestones. They are occasionally accompanied by sheaf-like malachite aggregates and colourless, scalenohedral calcite crystals. Other secondary minerals include chrysocolla, azurite, tenorite, pseudomalachite, cuprite and native copper.
Dioptase at Altyn-Tyube forms attractive specimens, with sharp green crystals, sometimes up to 3 cm in size, in thick blankets over a characteristic white to brownish veined limestone (MinRec 54.2.209-253).
Dioptase from Altyn-Tyube - Image

At the Tsumeb Mine, Tsumeb, Oshikoto Region, Namibia, dioptase was found abundantly; beautiful, lustrous, transparent, dark emerald-green crystals on white calcite crystals are considered the world’s finest for the species. Dioptase crystals have been found up to 5 cm in size, and crystals around 1 cm are fairly common. Associated minerals besides calcite and dolomite include conichalcite, duftite, mottramite, malachite, cuprite, cerussite, plancheite, shattuckite, wulfenite and molybdofornacite. Attractive dioptase clusters with “snowfall” coatings of white minrecordite are also known (Minrec 55.6 supplement p95).
Dioptase from Tsumeb - Image

At the Renéville Mine, Renéville, Kindanba District, Pool Department, Republic of the Congo, dioptase is found as crystalline masses and geodes, some of which can reach 50 cm in their longest dimension. The individual crystals, sometimes doubly terminated, rarely exceed 3 or 4 cm. They occur associated with many minerals including plancheite, cerussite, cuprite, mottramite, fornacite, chrysocolla, azurite, malachite, wulfenite, pyromorphite, chalcocite, quartz and calcite.
In general, dioptase crystals from Renéville occur in vugs in massive dioptase lenses, the vugs commonly lined by baby-blue chrysocolla. The dioptase crystals are bright green, but sometimes with a mottled appearance because of cloudy inclusions, and lack the uniform very dark green tones of Tsumeb dioptase (MinRec 55.4.425-433).
Dioptase from Renéville - Image

At the Magma mine, Pioneer District, Pinal county, Arizona, USA, dioptase has been found associated with minor amounts of chrysocolla, azurite, malachite and olivenite, and occasionally crystals of wulfenite and cerussite to 2 mm (R&M 95.1.84).
Dioptase from the Magma Mine - Image

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