According to deformed specificities for rock mass bedding slope
the mode amplitude equation of equilibrium stability built by energy criterion of post-buckling are used
and nearby region at bifurcation point and cracking criterion at bedding slope end are derived. In accordance with mechanism for progressive failure of rock mass bedding slope and characteristic for rheologic deformation
various possible factors affected mode amplitude are analysed; and extremum of mode amplitude of equilibrium stability is given in the form of slope length.