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Pyromorphite - Santa Eufemia, Cordoba, Spain.jpg
CategoryPhosphate mineral
Apatite group
(repeating unit)
IMA symbolPym[1]
Strunz classification8.BN.05
Crystal systemHexagonal
Crystal classDipyramidal (6/m)

(same H-M symbol)
Space groupP63/m
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
Mohs scale hardness3.5-4
LusterResinous to subadamantine
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
Ultraviolet fluorescenceMay fluoresce yellow to orange under LW and SW UV
Other characteristicsPiezoelectric if biaxial

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. It is part of a series 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).

The phosphate was first distinguished chemically by M. H. Klaproth in 1784,[5][6][7][8] and it was named pyromorphite by J. F. L. Hausmann in 1813.[9][10] The name is derived from the Greek for pyr (fire) and morfe (form) due to its crystallization behavior after being melted.[3]

Paecilomyces javanicus is a mold collected from a lead-polluted soil that is able to form biominerals of pyromorphite.[11]

Properties and isomorphism[edit]

The color of the mineral is usually some bright shade of green, yellow or brown, and the luster is resinous. The hardness is 3.5 to 4, and the specific gravity 6.5 - 7.1. Owing to isomorphous replacement of the phosphorus by arsenic there may be a gradual passage from pyromorphite to mimetite. Varieties containing calcium isomorphously replacing lead are lower in density (specific gravity 5.9 - 6.5) and usually lighter in color; they bear the names polysphaerite (because of the globular form), miesite from Mies in Bohemia, nussierite from Nuizière, Chénelette, near Beaujeu, Rhône, France, and cherokine from Cherokee County in Georgia.[citation needed]


See also[edit]


  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85: 291–320.
  2. ^ Handbook of Mineralogy (PDF).
  3. ^ a b "Pyromorphite". Webmineral data.
  4. ^ "Pyromorphite".
  5. ^ Klaproth (1784). Von dem Wassereisen, als einem mit Phosphorsäure verbundenen Eisenkalke (in German). On hydrosiderum [i.e., iron phosphide, Fe2P] as a calcined [i,e, roasted] iron [that is] bonded with phosphoric acid), Chemische Annalen für die Freunde der Naturlehre … , 1 (5) : 390–399. From p. 394: After remarking that lead ores that contain phosphorus can be treated with strong acids to produce phosphoric acid, Klaproth notes that: " … wie solches zuerst Hr. Gahn in Schweden entdeckt, ich selbst aber bey Unersuchung des krystallisirten grünen Bleyerzes von der heil. Dreyfaltigkeit zu Zschopau bestätigt gefunden habe." ( … as such Mr. Gahn in Sweden first discovered, I myself, however, have found [to be] confirmed by investigation of the crystallized green lead ore [i.e., pyromorphite] from the Holy Trinity at Zschopau in Germany]
  6. ^ Details of Klaproth's chemical analysis of pyromorphite appear in: Klaproth (1785) "Ueber die Phosphorsäure im Zschopauer grünen Bleyspathe" (On phosphoric acid in green lead spar from Zschopau), Beyträge zu den chemischen Annalen, 1 (1) : 13–21.
  7. ^ LXXXVII. Chemische Untersuchung der phosphorsauren Bleierze: I. Zeisiggrünes Bleierz von Zschopau. (87. Chemical investigation of the lead ores [containing] phosphoric acid: I. Siskin-green lead ore from Zschopau) in: Klaproth, Martin Heinrich, Beiträge zur chemischen Kenntnis der Mineralkörper [Contributions to our chemical knowledge of minerals]. Vol. 3. Posen, (Germany): Decker und Co. ; Berlin, Germany: Heinrich August Rottmann. 1802. pp. 146–153.
  8. ^ Dr. Thomas Witzke. "Entdeckung von Pyromorphit (Discovery of pyromorphite)" (in German).
  9. ^ Hausmann, Johann Friedrich Ludwig (1813). Handbuch der Mineralogie. Göttingen, Germany: Vandenhoeck und Ruprecht. pp. 1090–1093.
  10. ^ Chester, Albert Huntington (1896). A Dictionary of the Names of Minerals Including Their History and Etymology. New York, New York: John Wiley & Sons. p. 224.
  11. ^ Young Joon Rheea; Stephen Hillier; Helen Pendlowskic; Geoffrey Michael Gadd (October 2014). "Fungal transformation of metallic lead to pyromorphite in liquid medium". Chemosphere. 113: 17–21. Bibcode:2014Chmsp.113...17R. doi:10.1016/j.chemosphere.2014.03.085.

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