The results of a study of the dispersed composition of muscovite micas and wollastonite, the shape of the particles of which are characterized by significant anisometry, are presented. A simple method of sedimentation analysis is proposed, which makes it possible to quickly, and most importantly, with high accuracy, determine the distribution of particles by their sedimentation diameters. Dependences have been obtained, with the help of which it is possible to calculate the geometric dimensions of the particles of the materials under study. Il. 4, bibliography: 5 titles.