exact location of the quarry is not known, waste layers of an old coticule quarry in the region of Vielsalm
Natural color
pale yellow coticule layer within purplish grey phyllite (slate)
Aged color
Components
phyllosilicates; garnets
Texture
Structure
Weathering
Diagnostic features
conspicuous fine-grained yellow coticula
Additional information
sample RD29; coticule is known for famous Belgian whetstone production; coticule is chiefly composed of crystals of spessartine and a K-mica rich matrix and very fine grains of quartz (grain size below 1 μm) (Goemaere et al. 2016)
Goemaere E., Demarque S., Dreesen R., Declercq P.-Y. 2016. The Geological and Cultural Heritage of the Caledonian Stavelot-Venn Massif, Belgium, Geoheritage 8: 211-233.