Mineral Database (Saesneg yn unig)

Mineral Database (Saesneg yn unig)

Tephroite

Crystal System: Orthorhombic
Formula: Mn2SiO4
Status of Occurrence: Confirmed Occurrence - 1st UK recording
Distribution: Locally Abundant
Chemical Composition: Manganese silicate
Method(s) of Verification: Benallt Mine - XRD (NHM, x2979, x3017, x3019, x3020, x3021, x13061 & x19405 & National Museum of Wales, NMW X-1487, 1497 & 1498); Nant Mine - XRD (National Museum of Wales, NMW X-1528, 1604, 1607, 1612 & 1615)
Chemical Group:
  • Silicates
Geological Context:
  • Metamorphic : low-grade
  • Metamorphic : skarn mineralization
Introduction: tephroite belongs to the broad olivine group of minerals and forms a series with the iron-rich olivine fayalite (Fe2SiO4). It is a typical mineral of iron-manganese ore deposits or their associated skarns, and in metamorphic rocks derived from manganese-rich sediments (Deer at al., 1982). It is associated with minerals such as rhodonite, bustamite, manganocalcite, hausmannite and spessartine.
Occurrence in Wales: tephroite is known from just one locality in Wales, although this represents the first recording of the mineral in the British Isles (Campbell Smith et al., 1944b).
Key Localities:
  • Benallt Mine, Llŷn, Gwyneddŷ: tephroite was identified from Benallt Mine where it is intimately associated with alleghanyite, and forms composite, dark, narrow, blade-like crystals up to 20 mm in length and varying in thickness from 2 mm down to microscopic sizes (Campbell Smith et al., 1944b). The crystals are olive-green in thin section and are elongated parallel to the c-axis. Tephroite was found ‘on the footwall side of no.1 ore-body by no. 1 Chute, 50-60 feet west of the main shaft, and some 10-29 feet above the 130-foot level’ (Campbell Smith et al., 1944b). A second locality within the mine was also recorded by these workers, ‘near the foot-wall of no.2 ore-body, located 40 to 80 feet west of the Court Shaft’.
  • Nant Mine, Nant-y-Gadwen, Rhiw, Llŷn, Gwynedd: tephroite is also a major component of massive siliceous manganese ore from the geologically similar Nant Mine (Cotterell, 2006). Typical examples are olive-green to chocolate-brown in colour and associated with jacobsite.
References:
  • Campbell Smith, W., Bannister, F.A. & Hey, M.H., 1944b Banalsite, a new barium-feldspar from Wales.  Mineralogical Magazine 27, 33-47
  • Cotterell, T.F., 2006 Caryopilite and pyroxmangite from Nant Mine, Nant-y-Gadwen, Llanfaelrhys, Pen Llyn, Gwynedd, Wales  UK Journal of Mines and Minerals, 27, 51-53.
  • Deer, W.A., Howie, R.A. & Zussman, J., 1986 Rock-Forming Minerals, Vol. 1A, Orthosilicates, 2nd Ed.  Longman Group Ltd, 918pp.