Cotunnite

Cotunnite
Cotunnite
General
Category	Halide mineral
Formula (repeating unit)	PbCl2
IMA symbol	Cot[1]
Strunz classification	3.DC.85
Crystal system	Orthorhombic
Crystal class	Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m)
Space group	Pnam
Unit cell	a = 7.6222(5) Å, b = 9.0448(7) Å, c = 4.5348(4) Å; Z = 4
Identification
Color	Colorless to white, pale green, pale yellow
Crystal habit	As elongated, flattened prismatic crystals; in aggregates of radiating sprays; granular, crustiform or pseudomorphs
Cleavage	Perfect on {010}
Fracture	Subconchoidal
Tenacity	Slightly sectile
Mohs scale hardness	2.5
Luster	Adamantine, silky to pearly
Diaphaneity	Transparent to opaque
Specific gravity	5.80
Optical properties	Biaxial (+)
Refractive index	nα = 2.199 nβ = 2.217 nγ = 2.260
Birefringence	δ = 0.061
2V angle	Measured: 67°
Solubility	Slight in water
References	[2][3][4]

Cotunnite is the natural mineral form of lead(II) chloride with formula PbCl₂.

It was first described in 1825 from an occurrence on Mount Vesuvius, Naples Province, Campania, Italy.^[3] It was named for Domenico Cotugno (Cotunnius) (1736–1822), Italian physician and Professor of Anatomy.^[2]

It was first recognized in volcanic fumarole deposits. It occurs as a secondary alteration product in lead ore deposits. It has also been reported as an alteration of archaeological objects that contain lead.^[2][5]

It occurs in association with galena, cerussite, anglesite and matlockite in the Caracoles, Chile. At the Tolbachik volcano on the Kamchatka Peninsula, Russia it occurs with the rare to uncommon minerals tenorite, , , , , , , halite, sylvite and native gold.^[2]

References[]