Class : Phosphates, arsenates, vanadates
    Subclass : Anhydrous phosphates
    Crystal system : Hexagonal
    Chemistry : Pb₅(PO₄)₃Cl
    Rarity : Common

Pyromorphite is a secondary mineral that occurs in the oxidation zones of lead deposits, the phosphorus required for its formation come from the apatite of nearby rocks. It belongs precisely to the apatite super group and constitutes the phosphorus pole of the pyromorphite-mimetite-vanadinite series. Its name comes from Greek puros (fire) and morphê (shape) because of the look taken by the melted crystals. The pyromorphite occurs in variable colors sometimes bright : yellow, orange, brown or green. The crystals are generally hexagonal, often cavernous, and can evolve to the acicular facies, sometimes botryoidal. Due to its beautiful colors, the pyromorphite is highly coveted by mineral collectors, it is also a secondary lead ore.

Pyromorphite is very present on the French territory which counts among the best deposits of the world with notably famous Les Farges Mine in Corrèze department which produced beautiful cavernous crystals up to 3 cm in size with an olive green to bright green color, sometimes brown (photo on the right). The old mine of Huelgoat in Finistère department gave big brown crystals and the small mine of Vézis crystals of 2 cm. More anecdotal, it is also necessary to note the deposits of Asprières (Aveyron), St-Salvy (Tarn), Pontgibaud (Puy-de-Dôme), Echassières (Allier), etc...

Two twins exist for pyromorphite mineral species but they are very rare and hardly observable.

The pyromorphite crystals can sometimes be replaced by galena (pseudomorphs), especially on the German and Breton deposits. A very beautiful Chinese discovery of 2015 reported large crystals, up to 5 cm, transformed into pale blue plumbogummite (right picture). Great groups have been able to make pieces of several kilos.

No fake recorded for this mineral species.