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wulfenite is a supergene lead mineral, typically encountered in the oxidation zones of veins, stockworks, disseminated and stratabound ore deposits in which galena and other primary lead minerals occur. The molybdenum may be supplied by molybdenum-bearing primary minerals such as molybdenite but in many cases, in which primary molybdenum is not present in sufficient quantity, it may be supplied by pervasive leaching of the wallrocks hosting the mineralisation. The classic associate of wulfenite is pyromorphite, but it may occur in association with a wide range of supergene minerals, particularly carbonates, phosphates and silicates. Wulfenite is an extremely stable mineral that tends to occur in fairly evolved supergene assemblages, characteristically in association with pyromorphite and cerussite as in the majority of its Central Wales occurrences (Mason, 2004). The associated species help with identification but the key is its distinctive crystal morphology and colour.
the first record of wulfenite in Wales, from Treffgarne Rocks in Pembrokeshire, was made as long ago as 1866, by Spencer George Percival. However, this was an erroneous identification - the mineral proving instead to be brookite - and it was not until just over 100 years had passed that the first authenticated occurrence, in Central Wales, was described (Ryback & Saville, 1967). Since that time, growing interest in the minerals of Wales has led to a minor flood of new occurrences: a review by Rothwell & Mason (1992) listed 22 Welsh localities and in the years since the list has grown to 29, including some important material in specimen terms. The majority of the localities (22 out of 29) are in the Central Wales Orefield.