The ripple topography of ion-beam-eroded surfaces offers a novel method to
determine the shape of collision cascades and the distribution of deposited
energy From the energy dependence of the ripple spacing of Ar+ and Xe+-irr
adiated graphite surfaces at ion energies between 2 and 50 keV, the relatio
ns between mean depth, longitudinal and lateral straggling of the damage ca
scade were obtained. Their evolution with the ion energy was found to follo
w power laws for both ion masses and implies an energy-independent lateral
spread of the damage cascade, while depth and longitudinal spread scale wit
h the ion energy. This can be explained by the nuclear stopping power being
nearly independent of energy in the observed region. High-resolution micro
graphs of single-ion impacts support this interpretation, as the hillock-sh
aped surface defects found in the experiments show a lateral extension bein
g independent of the ion energy.