Molecular dynamics simulations of the Oeffner-Elliot model of germania (GeO(2)) are performed to identify nested regions of anomalous behavior in structural order, diffusivity, and pair entropy in the density-temperature plane, analogous to that seen in BeF(2), SiO(2), and H(2)O. The decreasing constraint of local tetrahedrality in GeO(2), compared to SiO(2) and BeF(2), substantially lowers the onset temperatures for anomalous behavior relative to the experimental melting temperatures (T(m)). Germania resembles water, more strongly than the ionic melts, in terms of temperatures for onset of anomalous behavior as well as in the order maps; for example, the structural anomaly sets in at 3.42T(m) in BeF(2), 3.09T(m) in SiO(2), 1.43T(m) in GeO(2), and 1.21T(m) in H(2)O. The detailed shapes of the anomalous regimes vary for different systems but the relative temperatures of onset for different anomalies are very similar in the different systems. The pair correlation entropy is shown to be a crucial and experimentally accessible quantity for relating structure, entropy, and diffusivity that could be potentially useful for a large class of inorganic ionic liquids.