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Crystal System: Monoclinic
Status of Occurrence: Confirmed Occurrence
Distribution: Rare
Chemical Composition: Lead copper selenide selenate hydrate
Chemical Formula: Pb2Cu2(Se+3O3)(Se+6O4)(OH)4
Method(s) of Verification: Llechweddhelyg Mine – XRD & EMPA at the NHM (Rust, 1990); Frongoch Mine – XRD & EMPA (Green et al., 1996) substantial selenium is recorded, but exact proportions are unsure; Esgair Hir Mine - XRD (NHM, 7157F).

Chemical Group:

Geological Context:

Minute spherical schmiederite aggregates from Llechweddhelyg Mine, Central Wales Orefield. Field of view 3 mm wide. National Museum of Wales Collection (NMW 90.14G.M.223). Photo D.I. Green, © National Museum of Wales.
Velvety blue schmiederite from Llechweddhelyg Mine in the Central Wales Orefield. Specimen and photo S.A. Rust. © S.A. Rust.
Introduction: schmiederite is a secondary mineral found in the oxidized zone of lead- and copper-bearing ore bodies. It has a similar X-ray diffraction pattern to linarite, with which it forms a series, therefore electron microprobe analysis is required for definitive identification.
Occurrence in Wales: schmiederite has been reported from a number of mines in the Central Wales Orefield and from Machen Quarry in South Wales, but in many instances the actual mineral is linarite which forms a series with schmiederite and which is similar in appearance and crystal structure. Llechweddhelyg Mine represents the only fully verified locality. Re-examination of specimens and X-ray films from Eaglebrook Mine, Dyfngwm Mine and Machen Quarry suggest that linarite is more likely.

Key Localities:


  1. Green, D.I., Rust, S.A. & Mason, J.S., 1996. Classic British mineral localities: Frongoch Mine, Dyfed. UK Journal of Mines & Minerals, 17, 29-38.
  2. Rust, S.A., 1990b. Susannite and sulphatian schmeiderite from Llechwedd Helyg Mine, Tir-y-Mynach, Dyfed, Wales. U.K. Journal of Mines and Minerals, 8, 48