We have studied the condensation of Fe on Cu(111) at room temperature, 420 and 570 K in the coverage range 0.03–4 monolayers and using an Fe flux between 0.005 and 0.1 monolayer/s. The Fe deposit grows in form of flat three-dimensional islands, whose height increases with increasing substrate temperature. In contrast to the existing literature, layer-by-layer growth was never observed. The shapes of the islands and step heights strongly support the growth of fcc crystallites, which are in registry with the Cu(111) substrate.
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