Mineral Database (Saesneg yn unig)

Mineral Database (Saesneg yn unig)

Staurolite

Crystal System: Monoclinic
Formula: (Fe,Mg)4Al17(Si,Al)8O45(OH)3
Status of Occurrence: Confirmed Occurrence
Distribution: Locally Abundant
Chemical Composition: Iron magnesium aluminium silicate hydroxide
Method(s) of Verification: all cited occurrences - polarizing microscope
Chemical Group:
  • Silicates
Geological Context:
  • Sedimentary : allogenic (detrital)
Introduction: staurolite is a metamorphic mineral which is found in pelitic schists and gneisses formed under medium grade (amphibolite facies) conditions. Staurolite is typically Fe-rich in composition, with magnesium-rich staurolite only being stable under a restricted range of high P-T conditions in quartz-free rocks (Deer et al., 1992). Staurolite is a durable minerals and is consequently found as detrital grains in sediments.
Occurrence in Wales: no primary metamorphic occurrences of staurolite are known from Wales as amphibolite-grade metamorphic rocks are limited in distribution, being restricted to the Coedana Complex gneisses of Anglesey (Horák, 1993). The presence of detrital staurolite grains has been reported from glacial sands from several separate localities around Wales (Greenly, 1919, Griffiths, 1939, Griffiths & Stuart, 1940), indicating that the source of staurolite lay in a metamorphic terrain outside Wales.
Key Localities:
  • Ludchurch, Pembrokeshire: Griffiths & Stuart (1940) reported detrital staurolite from from the glacial deposits at Ludchurch in Pembrokeshire.
  • South Wales: staurolite was identified as a major component of the Irish Sea Drift in the region between Afon Neath and Afon Tywi (Griffiths, 1939).
  • Ty’n-ycaeau, near Menai, Anglesey: Greenly (1919) reported staurolite in the heavy residues from glacial sands exposed around Ty’n-ycaeau, near Menai, on Anglesey.
References:
  • Deer, W.A., Howie, R.A. & Zussman, J., 1992 An Introduction to Rock-Forming Minerals.  Longman Scientific & Technical, 696pp.
  • Greenly, E., 1919 The Geology of Anglesey.  Memoirs of the Geological Survey of Great Britain, 980pp (2 volumes).
  • Griffiths, J.C., 1939 The mineralogy of the glacial deposits of the region between the Rivers Neath and Towy, South Wales.  Proceedings of the Geologists’ Association, 50, 433-462.
  • Griffiths, J.C. & Stuart, A., 1940 An occurrence of detrital diaspore in South Wales.  Geological Magazine, 77, 74-76.
  • Horák, J.M., 1993 The Late Precambrian Coedana and Sarn Complexes, Northwest Wales - a Geochemical and Petrological study.  Unpublished Ph.D. thesis, University of Wales, 415pp.