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CampyliteCampylite is a variety of the lead arsenate mineral mimetite which received the name from the Greek 'kampylos'- bent, on account of the barrel-shaped bend of its crystals. It has also been used as an alternate name for pyromorphite. Additional recommended knowledgeIt occurs in the upper lead deposits through the oxidation of galena or cerussite. The main deposits are Pribam in Bohemia and Dry Gill, Caldbeck, near Wigton, Cumbria, England. References
Categories: Lead minerals | Arsenate minerals |
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Campylite". A list of authors is available in Wikipedia. |