Azurite
The blue copper carbonate that slowly becomes the green one — which is why so many old skies have turned to foliage.
Azurite forms in the same weathered copper deposits as malachite and is the deeper blue of the two. The pair are almost always found together, and the reason is that azurite is the less stable: given time and moisture it converts to malachite, keeping the crystal shape and changing the colour entirely.
That conversion is visible in art. Azurite was the everyday blue of medieval and Renaissance painting — ultramarine being ruinously expensive — and a good deal of it has since turned green on the panel, which is why skies and robes in some old paintings are not the colour they were made.
How to identify it
Deep azure blue, with a light blue streak and a vitreous lustre, and it effervesces in dilute acid. It is soft, around 3.5 to 4, and commonly intergrown with green malachite — often as a blue core within green.
How we know: checked recently · only one source, so there is nothing to cross-check it against · stated directly by the source.
How this connects
Where a connection has been confirmed by an outside reference, that reference is named beside it.
is an ore of
- Copper — element · a minor secondary ore, almost always worked alongside malachite Wikidata
is an alternative to
- Chalcopyrite — mineral · the same substitution as malachite and for the same reason — an oxidised copper carbonate leached rather than smelted, from the weathered cap of a sulfide deposit
- Malachite — mineral · the two oxidised copper carbonates, mined together and treated identically. Azurite is the less stable of the pair and slowly alters to malachite, which is why green outcrops are commoner than blue ones
is a component of
- Oxidised zone — deposit type · the blue one, less stable than malachite and slowly altering to it, which is why green outcrops outnumber blue
Sources
- Material WorldOur own writing
- Wikimedia Foundation · Creative Commons CC0 1.0 Universal (public domain dedication)
- COD Advisory Board / Vilnius University · CC0 — contributors place data in the public domain