  The Regge Calculus approximates a continuous manifold by a simplicial
lattice, keeping the connectivities of the underlying lattice fixed and taking
the edge lengths as degrees of freedom. The Discrete Regge model employed in
this work limits the choice of the link lengths to a finite number. This makes
the computational evaluation of the path integral much faster. A main concern
in lattice field theories is the existence of a continuum limit which requires
the existence of a continuous phase transition. The recently conjectured
second-order transition of the four-dimensional Regge skeleton at negative
gravity coupling could be such a candidate. We examine this regime with Monte
Carlo simulations and critically discuss its behavior.
