Revisiting Glacier Dynamics for Stationary Approximation of Plane-Parallel Creeping Flow

We have presented in this analytical research the revisiting of approach for mathematical modeling Glacier dynamics terms viscous-plastic theory 2-dimensional movements within (x, y)-plane cartesian coordinates. The stationary creeping approximation plane-parallel flow slowly moving glacial ice on absolutely flat surface without any inclination has been considered. Even such simple formulation, equations motion that governs by is hard to be solved analytically. succeeded obtaining expression components velocity Ox-direction (Ox-axis coincides initial main direction ice). Restrictions form stem from continuity equation as well special condition non-Newtonian (viscous-plastic) used insofar.