Within the framework of reinterpretation of the depositional evolution of the Komjatice depression. presence of cummingtonite in weakly lithified sediment has been detected. The sediment is formed by volcanic lithoclasts and phenocrysts with a small admixture of non-volcanic grains. The different mineral composition and various degrees of alteration of volcanic lithoclasts. https://www.espumasyterciopelo.com/product-category/ribbon/