The temperature and pressure derivatives of the elastic moduli M of solids can be cast into the form of dimensionless logarithmic anharmonic {DLA} parameters, a In M/8 In p = {M} at constant temperature, pressure, or entropy (T, P, S), where p 1s the density. These parameters show little variation from material to mat_erial and_ an'. expected t_o s?ow _little variation with temperature at high temperature. Most of the available denvatlve data for 10mc sohds has been renormalized and analyzed for dependency on 10n type, crystal structure, and other parameters. The {DLA} parameters exhibit little variation and little cNrelation with crystal structure for most close-packed halides and oxides. There are small systematic vanat10ns with 10mc radms, Griineisen's y, and the bulk modulus-rigidity ratio (K/G). Temperature and pressure derwatlves are correlated because of the importance of the volume-dependent, or extrinsic, terms. The mtnns1c terms { K}v and { G}v are also highly correlated, even for open-packed structures, where a In M/aaT = {M}v. These correlations make it possible to estimate the derivatives of highpressure phases. The spine! forms of olivine are predicted to have "normal" derivatives, and therefore the magnitude of the modulus or velocity jump associated with the olivine-spine! transition near 400 km should be similar to that measured in th~ laborat?~Y· The actual size of the 400-km discontinuity is much less, md1_catmg the presence of subst~ntial _quantlhes of mmerals other than olivine in the upper mantle or trans1t10n reg10n. Rece_nt calculat10ns m apparent support of a homogeneous olivine-rich (>60%) mantle are based on choices for the denvatJves of /3-and y-Mg 2 Si0 4 , which are unlike other ionic crystals. There is no evidence that these phases should be anomalous in their physical properties. The temperature and pressure derivatives of ionic crystals depend on the nature of the ions and their coordination.