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Campylite is a variety of the lead arsenate mineral Mimetite. It received its name from the Greek ‘kampylos’ meaning bent, on account of the barrel-shaped bend of its crystals. It occurs in the upper lead deposits through the oxidation of galena or cerussite. The main deposits are Pribam in Bohemia, Czech Republic, and Dry Gill, Caldbeck Fells, near Wigton, Cumbria, UK.
from Dry Gill Mine, Cumbria
ACTUAL AS SEEN: The image shows the EXACT specimen you will receive. The specimen has been carefully hand selected and photographed. Measurements are as accurate as possible, though be aware measuring precise dimensions can be difficult from irregular shaped items. Whilst we portray colours as close to life-like as we can, colours will vary if taken in sunlight, indoors, from monitor to monitor and device to device. Once this specimen is sold, we will update this listing with new similar selected item, with a new photo and dimensions.
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