By using the generalized cell mapping digraph (GCMD) method, we study
bifurcations governing the escape of periodically forced oscillators
in a potential well, in which a chaotic saddle plays an extremely
important role. In this paper, we find the chaotic saddle and we
demonstrate that the chaotic saddle is embedded in a strange fractal
boundary which has the Wada property, that any point on the boundary
of that basin is also simultaneously on the boundary of at least two
other basins. The chaotic saddle in the Wada fractal boundary, by
colliding with a chaotic attractor, leads to a chaotic boundary
crisis with a global indeterminate outcome which presents an extreme
form of indeterminacy in a dynamical system. We also investigate the
origin and evolution of the chaotic saddle in the Wada fractal
boundary, particularly concentrating on its discontinuous
bifurcations (metamorphoses). We demonstrate that the chaotic saddle
in the Wada fractal boundary is created by the collision between two
chaotic saddles in different fractal boundaries. After a final escape
bifurcation, there only exists the attractor at infinity; a chaotic
saddle with a beautiful pattern is left behind in phase space.