Zeolite refers to a family of naturally occurring microporous minerals known as hydrated aluminosilicates[1]. The term "zeolite" was coined in 1756 by Swedish mineralogist Axel Fredrik Cronstedt, who observed that a mineral (later identified as stilbite) released steam when heated – as if it were "boiling." Based on this behavior, Cronstedt named it zeolite from the Greek ζέω (zéō, "to boil") and λίθος (líthos, "stone"), literally meaning "boiling stone"[2].
Geological Formation
Natural zeolites like clinoptilolite formed millions of years ago in the Earth's crust. Most deposits originated when volcanic ash layers aged in the presence of alkaline water[4]. For example, volcanic ash settling in ancient lakes or marine basins gradually altered into zeolite minerals under low temperature and moderate pressure conditions. This process (a form of prolonged diagenesis) yielded thick sedimentary zeolite-rich rock strata over geologic time[5-6].
Many zeolite deposits date to the Cenozoic era (past ~65 million years), especially the Miocene epoch, though some formed in Mesozoic strata[7-8]. Natural zeolites are widespread in regions with past or current volcanic activity – they are found on every continent, from the Tanzawa Mountains of Japan to Yellowstone in the USA, and in volcanic tuffs across Europe[9-10].
Abundant mineable zeolite species include clinoptilolite (often occurring with its close cousin heulandite), mordenite, chabazite, analcime, and phillipsite, among others[11]. Today, these minerals are no longer obscure; they are actively mined in many countries for their valuable applications.