“…The literature on the cubic Si and Ge surfaces is very rich and particularly the low-index surfaces, such as the (001), the (110) and the (111) ones, are quite well understood [31][32][33]. The higher index surfaces, especially the (112) have received less consideration, mainly because it was often considered intrinsically unstable, suggesting that it decomposes into (111) and other high-index facets [34,35] at the termination of bulk-like samples. Whether the (112) sidewalls, which are clearly discernible in VLS grown Si NWs [36], are also composed by sawtooth structures including the (111) facets, or they have the nominal (112) orientation, is still not completely understood.…”