“…Certain planar interfaces of macroscopic single crystals can be thermodynamically induced to spontaneously decompose into fully faceted morphologies by thermal [16,17], chemical [7,[18][19][20][21] or electrochemical means [13,22]. Experimental observations of spinodally decomposing interfaces [23,24], such as those for thermally quenched Si(111) [17] or the oxygen-induced faceting of Cu(115) [19], reveal an ensuing coarsening of the resulting fully faceted interfaces, and the concomitant emergence of scaling regimes, wherein a power law governing the time t evolution of the characteristic length L of the interface's morphology appears [16,17],…”