We demonstrate that Ͼ1 m lateral scale atomic height range steps and terraces can be formed at the Si(001)-SiO 2 interface by annealing at high temperatures, such as 1325°C, in an Ar atmosphere containing a small fraction of O 2 . The kinetics of the step-terrace morphology formation are quantitatively consistent with a model in which Si is emitted from the interface during the annealing, diffuses in the oxide, and returns. The step-terrace morphology is a logical consequence of recent theoretically proposed ordered interfacial structures at this interface, supporting the structures' existence.