Massive quartz–chalcedony ± opal nodules (“plasma” in gemology) represent a specific silica variety, which occurs in the laterite-like residues of pre-Miocene paleo-weathering of ultramafites in western Moravia (Moldanubian Zone, Bohemian Massif). These zonal silica nodules (ZSN) tend to have concentric texture with a dark green to green-brown core, pale green margin and a narrow white rim (outer surface zone). The most typical microscopic feature of ZSN is vermiform microstructure particularly in the two outer zones. Individual zones consist of micro- to non-crystalline SiO₂ polymorphs with variable contents of H₂O (quartz, chalcedony, moganite, opal-C/CT and opal-A). The predominant green colour is due to submicroscopic smectite pigment, while the brownish colour originated from decomposition of smectite to iron oxohydroxides. ZSN formed in subaerial, partially reducing conditions in the lower part of weathering crusts covering serpentinites. The whole process was preceded by component exchange (chloritization) along serpentinite – felsic rocks (granulite, migmatite, pegmatite veins) boundaries. The gradual silica migration and subsequent redistri­bution associated with the removal of aluminium, magnesium and iron led up to the formation of a zonal nodular texture dominated by SiO₂ polymorphs. Newly formed minerals in micro-cavities and cracks of ZSN are represented by acces­sory pyrite and sporadic barite. Zonal silica nodules-bearing residues on serpentinites occur only in a narrow area which was originally covered by clay-sandy Miocene sediments of the Carpathian Foredeep in western Moravia. Probably late low-temperature fluid interaction between silicified serpentinite residuum (chlorite – montmorillonite saprolite) and marine sediments may be the main factor controlling formation of ZSN.