We study boundary crisis in quasiperiodically forced dissipative systems us
ing the Henon map as a characteristic example. The crisis is due to a homoc
linic tangency of the stable and unstable manifolds of an accessible invari
ant circle of saddle type on the basin boundary of the attractor Numerical
evidence shows that the type of boundary crisis can change as the saddle ci
rcle loses its accessibility due to the quasiperiodic forcing. This implies
the existence of codimension-two double crisis vertices where a curve of b
oundary crisis and a curve of interior crisis meet. We argue that bifurcati
on points of higher codimension must exist in the full parameter space. (C)
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