Anhydrous carbonate containing hydroxyl, copper mineral
Specific gravity: 3.77
Hardness: 3½ to 4
Streak: Light blue
Colour: Deep blue
Solubility: Azurite is moderately soluble in hydrochloric, sulphuric and nitric acid
Azurite is less common than malachite but has the same origin
It is a secondary mineral found largely in the oxidation portions of
It may be found in gneiss.
At the Chessy copper mines, Chessy-les-Mines, Villefranche, Rhône, Auvergne-Rhône-Alpes, France, azurite pseudomorphs after cuprite (KL p176), and malachite pseudomorphs after azurite have been found (R&M 95.3.275).
At Tsumb, Namibia, azurite is mostly partially or wholly altered to malachite; unaltered azurite crystals are much less common (R&M 93.6.540). Smithsonite and tennantite pseudomorphs after azurite have been found here (KL p1676, R&M 95.3.275).
At the Snelston mine, near Ashbourne, Derbyshire, England, UK, azurite is associated with malachite and cerussite in a sandstone matrix (RES p140,141).
At the Bardon Hill quarry, Coalville, Leicestershire, England, UK, azurite is associated with malachite in dacite (RES p193).
At the New Cliffe Hill quarry, Stanton under Bardon, Leicestershire, England, UK, azurite has been found associated with malachite and vésigniéite, and also with malachite, cuprite and native copper (RES p195, 196).
At Cloud Hill quarry, Breedon on the Hill, Leicestershire, England, UK, azurite has been found associated with chalcopyrite, goethite and dolomite (RES p208).
At the Westcott mine, Pulverbatch, Shropshire, England, UK, azurite has been found associated with chalcocite (RES p289).
At the Llynclys quarry, near Oswestry, Shropshire, England, UK, azurite has been found in cavities in chalcopyrite - goethite veinstone, with minor malachite (RES p294).
At Judkins quarry, Nuneaton, Warwickshire, England, UK, azurite has been found coating calcite (RES p294).
At the Campbell mine, Bisbee, Arizona, USA, malachite pseudomorphs after azurite have been found (KL p179).
At the Apex mine, Jarvis Peak, Beaver Dam mountains, Washington county, Utah, USA, an azurite and malachite pseudomorph after gypsum has been found (KL p177).
Azurite is formed by the action of carbonated water on copper-containing minerals, or from copper-containing solutions, such as CuSO4 or CuCl2 reacting with limestone.
azurite and H2O to malachite and CO2
2Cu3(CO3)2(OH)2 + H2O → 3Cu2(CO3(OH)2 + CO2
Azurite is unstable under atmospheric conditions, and slowly converts to the more stable malachite according to the above reaction.
The Activity-pH diagram below was calculated at 298.2 K for some carbonates and copper arsenates for constant activity (roughly equivalent to concentration) of H2AsO4- in solution, over a range of values of pH and of H2CO3 activity (MM 52.687).
The mineral formulae are:
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