Asteroids are believed to be remnant planetesimals from the crucial period of the planetary formation. The knowledge of their present properties can help us to understand the primordial processes which governed the evolution of the Solar System immediately after the collapse of the planetary nebula and before the formation of the planets. The mineralogy of their surfaces, the mechanisms of radiative transfer of the atmosphere-less bodies, the computing of their synodic periods, shapes and spins, as well as the “in situ” observations by spacecrafts, will help us to understand the asteroidal population. The lightcurves and synodical periods for 15 asteroids have been observed by photometrical and CCD photometry. By statistical analysis I foun...