The thermal expansion of a synthetic pyrolidine dodecasil-3C (D3C) cla
thrasil from 15 to 300 K has been determined from high-resolution diff
raction patterns obtained with synchrotron radiation. The thermal expa
nsivity is found to be significantly larger than that of alpha-quartz.
A larger thermal expansivity indicates greater anharmonicity in the i
nteraction potentials. This observation suggests that the clathrasils
may exhibit anomalous glassy solid behavior analogous to that found in
clathrate hydrates.