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Campylite

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Campylite
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Campylite 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.

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It occurs in the upper lead deposits through the oxidation of galena or cerussite. The main deposits are Příbram in Bohemia and Dry Gill, Caldbeck Fells, near Wigton, Cumbria, England.

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References

Further reading

  • Mick Cooper and Chris Stanley, 1990, Minerals of the English Lake District, Natural History Museum Publications, London, ISBN 0-11-310022-1


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