Pyromorphite

Pyromorphite
General
CategoryPhosphate mineral
Apatite group
FormulaPb5(PO4)3Cl
IMA symbolPym
Strunz classification8.BN.05
Crystal systemHexagonal
Crystal classDipyramidal (6/m)

(same H-M symbol)
Space groupP63/m
Identification
ColorDark green to grass-green or green, yellow, yellow-orange, reddish orange, yellow-brown, greenish-yellow or yellowish-green, shades of brown, tan, grayish, white and may be colorless; colourless or faintly tinted in transmitted light.
Crystal habitPrismatic to acicular crystals, globular to reniform
TwinningRarely on {1122}
CleavageImperfect- [1011]
FractureUneven to sub-conchoidal
TenacityBrittle
Mohs scale hardness3.5–4
LusterResinous to subadamantine
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity7.04 measured, 7.14 calculated
Optical propertiesUniaxial (−) May be anomalously biaxial (−)
Refractive indexnω = 2.058 nε = 2.048
Birefringenceδ = 0.010
PleochroismWeak
Ultraviolet fluorescenceMay fluoresce yellow to orange under LW and SW UV
Other characteristicsPiezoelectric if biaxial
References

Pyromorphite is a mineral species composed of lead chlorophosphate: Pb5(PO4)3Cl, sometimes occurring in sufficient abundance to be mined as an ore of lead. Crystals are common, and have the form of a hexagonal prism terminated by the basal planes, sometimes combined with narrow faces of a hexagonal pyramid. Crystals with a barrel-like curvature are not uncommon. Globular and reniform masses are also found.

Pyromorphite is part of the apatite group of minerals and bears a close resemblance physically and chemically with two other minerals: mimetite (Pb5(AsO4)3Cl) and vanadinite (Pb5(VO4)3Cl). The resemblance in external characters is so close that, as a rule, it is only possible to distinguish between them by chemical tests. They were formerly confused under the names green lead ore and brown lead ore (German: Grünbleierz and Braunbleierz).