Abstract
A large T3 specific-heat anomaly associated with a vibrational mode near 40 cm1 is found in cristobalite and vitreous silica, but not in quartz or g-B2 O3. A material-specific structural model is proposed for this anomaly. The model also explains the 40- and 80-cm1 modes observed by neutron scattering in cristobalite and g-SiO2 as well as the absence of dispersion in the hypersonic transverse sound velocity. Specific relations with recently observed anomalies in the 775-cm1 Raman band of mixed alkali silicates are suggested and specific experiments designed to test phase separation at the elemental molecular level (true spinodal decomposition) are proposed.