Mineral Database (Saesneg yn unig)

Mineral Database (Saesneg yn unig)
Mineralogy of Wales

Foitite

Crystal System: Hexagonal
Formula: (â–¡,Na)(Fe2+,Al)3Al6Si6O18(BO3)3(OH)4
Status of Occurrence: Confirmed Occurrence
Distribution: Uncommon
Chemical Composition: Sodium iron aluminium hydroxyborosilicate
Method(s) of Verification: Cwm Bychan - EMPA (National Museum of Wales & A.G. Tindle, unpublished data).
Chemical Group:
  • Silicates
Geological Context:
  • Igneous
Introduction: foitite is a tourmaline family mineral and belongs to the 'vacancy' group, based on the absence of atoms in the X site. The mineral can be further divided into fluor-, hydroxyl- or oxy varieties, depending on the filling of the W site in the crystals lattice (see tourmaline entry for more details).
Occurrence in Wales: although several occurrences of tourmaline have been reported from Wales (see tourmaline entry), a lack of detailed optical or analytical data has precluded most of these from being classified to mineral species level. New data (National Museum of Wales & A.G. Tindle, unpublished data) confirms the presence of foitite in at least one of these occurrences. As more microprobe data becomes available it is anticipated that a more widespread distribution of foitite in Wales will be demonstrated.
Key Localities:
  • Cwm Bychan, Beddgelert, Gwynedd: samples of Caradocian sandstone studied by Beavon (1963) (e.g. NMW 80.30G), held in the National Museum of Wales, contain aggregates of subhedral basal sections and prisms, showing concentric optical zoning. Microprobe analyses reveal these to be crystals of schorl and foitite, with outer rims of dravite.
References:
  • Beavon, R.V., 1963 The succession and structure east of the Glaslyn River, North Wales.  Quarterly Journal of the Geological Society of London, 119, 479-512.
  • Hawthorne, F. C. & Henry, D. J., 1999 Classification of the minerals of the tourmaline group.  European Journal of Mineralogy, 11, 201-215.