Crystal System: Hexagonal
Status of Occurrence: Confirmed Occurrence - 1st UK recording
Chemical Composition: Copper yttrium calcium arsenate hydroxide hydrate
Chemical Formula: (Y,Ca)Cu6(AsO4)3(OH)6.3H2O
Method(s) of Verification: Gwaith-yr-Afon Mine - XRD & EDX (National Museum of Wales).
- Supergene: post-mining oxidation & weathering deposits
Introduction: agardite is a rare mineral restricted in its occurrences to supergene alteration zones overlying polymetallic ore deposits in which arsenic is present. A wide range of other supergene minerals may be associated. It is related to, and resembles, mixite - in which bismuth takes the place of the rare earths. It also resembles finely fibrous pale malachite, and in consequence is not a particularly easy mineral to identify without using analytical techniques.
Occurrence in Wales: agardite-(Y) is only known from three UK localities - one in Wales and two in Cornwall. The Welsh occurrence is at Gwaith-yr-Afon Mine in Central Wales, where it occurs as a member of an unusually diverse arsenate assemblage in an area not generally known for its arsenic minerals (Rust & Mason, 1994).
- Gwaith-yr-Afon Mine, Goginan, Ceredigion: agardite-(Y) occurs rarely as tufts of minute (<0.25 mm) but lustrous deep to pale green acicular crystals on joints in mudstone breccia which are coated in friable black Fe-Mn oxides. Associated minerals are malachite and mimetite. The few specimens known were collected underground in the early 1990s.
There are no key localities for this specimen.
- Rust, S.A. & Mason, J.S., 1994. An unusual occurrence of arsenate minerals at Gwaith-yr-Afon mine, Dyfed, Wales. Journal of the Russell Society, 5(2), 109-113.
There are no references for this specimen.