THE ROTATION OF UNELASTIC EARTH Churkin V.A. Institute of Theoretical Astronomy, St-Petersburg, Russia Nowadays the rheological condition of the Earth's interior is known with great uncertainty. Therefore the influence of the rheo- logical qualities of the Earth on its rotation must be taken into consideration in the most general analytic form. In our opinion, linear integral operators are such analytical forms. In fact, in- tegral operators allow to account the most important quality of the unelastic mediums - the effect of the hysteresis loop or othe- rwise the effect of the phase lag of the unelastic medium's reac- tion on the external force, which with necessity leads to the dis- sipation of the mechanical energy. Besides, every integral opera- tor hides the rheological information in its nucleus. This allows to preserve the mentioned nucleus in the symbolic form when const- ructing the theory of the unelastic Earth rotation, and only on the finishing stages to reveal its analytical structure, thus fi- xing the concrete rheological qualities. In our work the initial well known algebraic equation, con- necting the angular velocity of the elastic body with its inertia moments, is replaced by the integral operator. On the base of this hypothesis the integro-differential equations of the Earth rotati- on, generalizing the differential equations of Eyler-Liuville, were obtained. Then, by using the Laplace-transformation the ini- tial system of integro-differential equations is solved in the general form (preserving the nucleus of the integral operator in the symbolic form) with respect to the Laplace-images of the com- ponents of the angular velocity. Inverse Laplace-transformation in this work we make for two types of nucleus of the integral opera- tor - for the nucleus of the Dirak Delta-function (which corres- ponds to the rheological model of the elastic Earth) and for the nucleus of the exponential type. In the context of these two types of nucleus of the integral operator the expressions for free and forced nutation of the Earth were obtained.