The present study examines various methods used for the characterization of three common natural silicate minerals, one zeolite (clinoptilolite) and two clays (montmorillonite and vermiculite). Characterization of natural minerals were performed through a series of analytical measurements so as gather all the information needed regarding their properties, in order to distinguish them from "similar" minerals such in the case of clinoptilolite vs heulandite and vermiculite vs hydrobiotite; this will enable their further use in environmental applications. The methods used in the present study are XRD, XRF, FTIR spectroscopy, TG/DTG/DTA and N2-porosimetry (BET). Data revealed from XRD, FTIR, TG/DTG/DTA showed that all three minerals have characteristic bands that can characterized and distinguish each other. The key difference between Heulandite and Clinoptilolite is their behavior upon heating. Clinoptilolite is stable at temperatures exceeding 450 o C, where heulandites undergo structural collapse below 450 o C. XRF analysis showed that Vermiculite sample is rich in MgO (Mg-vermiculite) and the low concentration of K2O revealed the presence of Vermiculite instead of Hydrobiotite. Thermogravimetric analysis showed that the main regions of Clinoptilolite weight loss are the release of looselybound water (50-200°C), release of "zeolitic" water (200-700°C) and finally the collapse of crystal structure (700-900°C). In the range 25-400 o C, the endothermal (DTA diagram) process of dehydration occurred in one step. This reveals the presence of clinoptilolite, because for heulandites dehydration occurs in two steps. As far as porosity is concerned, all three minerals are generally dominated by micro/mesopores. BET surface area for clinoptilolite is between 17-100 m2/g, for bentonite 22-42 m 2 /g and for vermiculite 7-18 m 2 /g. The acquired analytical results enabled the full characterization of the examined minerals, despite their common properties.