Mineral Database
Cotunnite
Crystal System: Orthorhombic
Formula: PbCl2
Status of Occurrence: Confirmed Occurrence
Distribution: Rare
Chemical Composition: Lead chloride
Method(s) of Verification: Penrhyn Du Mine - XRD at Manchester Museum (X-ray reference number MANCH:XRD727).
Chemical Group:
- Halides
Geological Context:
- Supergene : post-mining oxidation & weathering deposits
- Supergene : in situ natural oxidation & weathering deposits
Introduction:
cotunnite occurs as a volcanic sublimate and as an alteration product of galena under saline conditions.
Occurrence in Wales:
cotunnite has been described (Hubbard & Green, 2005) within weathered galena-rich veinstone from the phosgenite locality at Penrhyn Du on the Llŷn. It was found as bladed microcrystals in material collected in situ from a vein exposed below the High Water mark. It is likely that a reaction between chlorine in the seawater and lead within galena in the veinstone has produced this rare mineral.
Key Localities:
- Penrhyn Du, Abersoch, Llŷn, Gwynedd: cotunnite was described by Hubbard & Green (2005) forming whitish translucent tapering bladed crystals to 4 mm in a cavity in oxidized galena and was associated with a few tiny sulphur crystals. Hubbard & Green note that phosgenite is far more common than cotunnite at Penrhyn Du.
References:
- Cotunnite from Penrhyn Du Mine, Gwynedd, Wales. Journal of the Russell Society, 8(2), 106-107.
