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 between 6.5 and 7.1.13 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 Stříbro (pronounced Mies in German) in Bohemia, nussierite from Nuizière, Chénelette, near Beaujeu, Rhône, France, and cherokine from Cherokee County in Georgia.
Cornelius S. Hurlbut; W. Edwin Sharp (1998). Dana's Minerals and How to Study Them (After Edward Salisbury Dana). John Wiley & Sons. p. 216. ISBN 978-0-471-15677-2. 978-0-471-15677-2 ↩
Cornelis Klein; Barbara Dutrow (2007). Manual of Mineral Science. Wiley. p. 430. ISBN 978-0-471-72157-4. 978-0-471-72157-4 ↩
A. Bishop; A. Woolley; W. Hamilton (1999). Cambridge Guide to Minerals, Rocks and Fossils. Cambridge University Press. p. 88. ISBN 978-0-521-77881-7. 978-0-521-77881-7 ↩
Nicholas Eastaugh; Valentine Walsh; Tracey Chaplin; Ruth Siddall (2008). Pigment Compendium. Routledge. p. 320. ISBN 978-1-136-37392-3. 978-1-136-37392-3 ↩
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] https://books.google.com/books?id=lqU5AAAAcAAJ&pg=PA390 ↩
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. https://books.google.com/books?id=NYjBkHlP7CIC&pg=RA1-PA13 ↩
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. https://books.google.com/books?id=8A8KAAAAIAAJ&pg=PA146 ↩
Dr. Thomas Witzke. "Entdeckung von Pyromorphit (Discovery of pyromorphite)" (in German). http://tw.strahlen.org/typloc/pyromorphit.html ↩
Hausmann, Johann Friedrich Ludwig (1813). Handbuch der Mineralogie. Göttingen, Germany: Vandenhoeck und Ruprecht. pp. 1090–1093. https://babel.hathitrust.org/cgi/pt?id=nyp.33433062733062;view=1up;seq=1114 ↩
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. https://books.google.com/books?id=IiwFAAAAMAAJ&pg=PA224 ↩
"Pyromorphite". Webmineral data. http://webmineral.com/data/Pyromorphite.shtml ↩
Rhee, Young Joon; Hillier, Stephen; Pendlowskic, Helen; Gadd, Geoffrey Michael (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. PMID 25065784. Retrieved 2024-11-12. /wiki/Geoffrey_Michael_Gadd ↩