Ion exchange properties of Georgian analcime, phillipsite and scolecite have been studied. The exchange capacity of analcimes is higher for sodium cations, decreasing in the following series: Na >K >Ag >NH4 >Ca 2>Sr 2>Li , the selectivity sequence for the sodium-enriched form is NH4 >Ag >Li >Ca 2>K ~Sr 2. For phillipsite ion exchange isotherms prove the high selectivity towards NH4 and K depending on the origin of zeolite: K >NH4 >>Ca 2>Mg 2 for samples with comparatively low content of potassium, and NH4 >K >Na >>Ca 2>Mg 2 for samples with high K-content. For scolecite selectivity sequences depend on temperature and flow rate, at low temperatures and under static conditions the selectivity sequence is Sr 2 >Ba 2 >Rb >Ca 2 >Cs >K >NH4 >Na >Mg 2 >Li >Cd 2>Cu 2 >Mn 2 >Zn 2 >Co 2 >Ni 2.