You are here:  >   >   >   >   >   > 
Cymraeg

Scorodite

Crystal System: Orthorhombic
Status of Occurrence: Confirmed Occurrence
Distribution: Locally Abundant
Chemical Composition: Hydrated iron arsenate
Chemical Formula: FeAs04.2H20
Method(s) of Verification: Tan-y-garth - XRD (National Museum of Wales, NMW X-103); all other occurrences reported are based on visual identifications

Chemical Group:

Geological Context:

Scorodite forming a microcrystalline crust. Bethesda. National Museum of Wales Collection (NMW 78.85G.M.20). Photo D.I. Green. © National Museum of Wales.
Introduction: scorodite is a common supergene mineral in areas where primary arsenopyrite-bearing mineralization is present. It may be the only supergene species present, or in more evolved oxidized deposits it may occur accompanied by pharmacosiderite and a range of base-metal arsenates (depending upon the geochemistry of the primary sulphide mineralization). It occurs typically associated with part-weathered, crumbly and cracked arsenopyrite, as pale greenish-yellow discernably crystalline crusts. The association with this matrix is often diagnostic in identifying the material as scorodite.
Occurrence in Wales: as arsenopyrite is widespread and locally common in Wales, it is perhaps unsurprising that quantities of scorodite have been found at a number of localities. In all of these, it is thought to be post-mining in origin. First reported by Gilbey (1968) from the Dolgellau Gold-belt, it has since been noted from three other Welsh mining districts, namely the Snowdon Caldera, the Central Wales Orefield and the Dolaucothi gold mine. None of the known localities have produced scorodite in specimens of anything more than academic quality.

Key Localities:

There are no key localities for this specimen.

References:

  1. Bevins, R.E. & Mason, J.S., 1998. Welsh Metallophyte and metallogenic evaluation project: Results of a Minesite Survey of Gwynedd. National Museums of Wales, Cardiff.
  2. Gilbey, J.W., 1968. The mineralogy, paragenesis and structure of the ores of the Dolgellau Gold Belt, Merionethshire, and associated wall rock alteration. Unpublished Ph.D thesis, University of London, UK.
  3. 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.