To use all functions of this page, please activate cookies in your browser.
my.chemeurope.com
With an accout for my.chemeurope.com you can always see everything at a glance – and you can configure your own website and individual newsletter.
- My watch list
- My saved searches
- My saved topics
- My newsletter
ConnelliteConnellite is a very rare mineral species, a hydrous copper chloro-sulfate, Cu19Cl4(SO4)(OH)32·3H2O, crystallizing in the hexagonal system. It occurs as tufts of very delicate acicular crystals of a fine blue color, and is associated with other copper minerals of secondary origin, such as cuprite and malachite. Its occurrence in Cornwall was noted by Philip Rashleigh in 1802, and it was first examined chemically by Arthur Connell in 1847. Outside Cornwall it has been found only in Namaqualand in South Africa and at Bisbee, Arizona (USA) Additional recommended knowledgeThe type locality is Wheal Providence at Carbis Bay in Cornwall.[1] References
This article incorporates text from the Encyclopædia Britannica Eleventh Edition, a publication now in the public domain. Categories: Copper minerals | Halide minerals | Sulfate minerals |
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Connellite". A list of authors is available in Wikipedia. |