  We have studied the time evolution of magnetization of a high spin magnetic
cluster in the ground state, in the presence of a sinusoidal axial magnetic
field and a static transverse field by explicitly solving time dependent
schr\"odinger equation. We observe oscillations of magnetization in the plateau
region which has all the characteristics reminiscent of the oscillation of
probability of occupation of a state in a two level lattice in the presence of
an oscillating electric field. The high spin of the ground state leads to a
large but finite two-level pseudo-lattice. The oscillations in magnetization
occur at amplitude of magnetic fields achievable in a laboratory and they also
persist for a wide range of spin-dipolar interactions.
  Thus, our study provides a magnetic analog of the optical two-level lattice.
