Crystal System: Not known
Status of Occurrence: Discredited Occurrence
Chemical Composition: Telluride of bismuth and silver
Chemical Formula: a mixture of Ag2Te and Bi4Te3
Method(s) of Verification: species discredited
Introduction: first described from a locality in Hungary by the mineralogist J.J. Huot in 1841, 'wehrlite' has since been shown to be an intimately intergrown mixture of the bismuth telluride pilsenite and the silver telluride hessite, and is thus no longer a valid mineral species (Ozawa & Shimazaki, 1982).
Occurrence in Wales: the presence of the now discredited mineral 'wehrlite' was recorded in galena dominated gold-bearing veins at Clogau Mine by Naden (1988).
There are no key localities for this specimen.
- Naden, J., 1988. Gold mineralisation in the Caledonides of the British Isles with reference to the Dolgellau Gold Belt and the Southern Uplands of Scotland. Unpublished Ph.D thesis, University of Aston, UK.
- Ozawa, T. & Shimazaki, H., 1982. Pilsenite redefined and wehrlite discredited. Proceedings of the Japanese Academy, 58, 291.