  In this paper the model for the neolithic migration in Europe is developed.
The new migration equation, the modified Klein Gordon equation is formulated
and solved. It is shown that the migration process can be described as the
hyperbolic diffusion with constant speed. In comparison to the existing models
based on the generalization of the Fisher approach the present model describes
the migration as the transport process with memory and offers the possibility
to recover the initial state of migration which is the wave motion with finite
velocity.
