Phosphate of copper
Cornetite is a phosphate of copper with hydroxyl, named after the geologist Jules Cornet [fr]. It was discovered in 1917.
Type locality
Cornetite is most notably found in the Star of Congo mine, near Lubumbashi.
Environment
Cornetite is a rare secondary mineral in some hydrothermal copper deposits.
Structure
Unlike related phases such as pseudomalachite, the copper atoms are all five-fold coordinated by oxygen. There are three unique copper sites that are all quite distorted from ideal symmetry. Two are in approximate tetragonal pyramids and the third is essentially a trigonal bipyramidal coordination. Edge sharing polyhedra lead to copper-copper dimer formation, and the overall structure is a three-dimensional network of copper-oxygen polyhedra.[5]
References
Wikimedia Commons has media related to
Cornetite.