These deposits are assigned to the Diest Formation, but this has recently been questioned (Houthuys, 2014). In some cases, silex pieces are present in the stones. This variety is called 'Puddingstone of Ronse' or 'Poudinge de Renaix'
quartz (mono- and polycrystalline) and glauconite (up to 50%, often altered to iron(hydr)oxides), minor amount of muscovite; cement of iron(hydr)oxides (limonite);high intergranular porosity
Texture
fine grain size; well sorted; sub-angular quartz and rounded glauconite grains
Houthuys R. 2014. A reinterpretation of the Neogene emersion of central Belgium based on the sedimentary environment of the Diest formation and the origin of the drainage pattern. Geologica Belgica 17, 3/4: 211-235.