In the dynamical triangulation model of 4D Euclidean quantum gravity w
e measure two-point functions of the scalar curvature as a function of
the geodesic distance. To get the correlations it turns out that we n
eed to subtract a squared one-point function which, although this seem
s paradoxical, depends on the distance. At the transition and in the e
longated phase we observe a power law behaviour, while in the crumpled
phase we cannot find a simple function to describe it.