Scapolite occurs as large idiomorphic crystals forming pseudoradiating aggregates in veins in the monzonitic rocks. It is associated with zeolites (analcime, natrolite and scolecite), calcite, ferroanchlorites, K-feldspar, sphene and apatite. The samples were examined by optical methods and chemical tests. The results define the mineral as a $Me_{36}$ scapolite term, containing $C0_{3}$ and OH as essential constituents and Cl and $SO_{4}$ as trace.