We present in-situ x-ray scattering measurements performed during the growth of two rare-earth metals, gadolinium and samarium, onto molybdenum (110) single crystals. The results have been interpreted using a diffusive growth model to determine the degree of interlayer mass transport in the initial stages of deposition. Both elements are shown to grow generally in a layerwise manner but with significant roughness after the initial layer is complete. A raised substrate temperature modifies the growth; the best Gd single layer is produced at a temperature of 140°C when deposited at a rate of 0.067 monolayers/min while for Sm the growth becomes increasingly islanded at higher temperatures. The presence of oxygen at the surface encourages layer-by-layer growth for both Gd and Sm, although a significant proportion of the atoms are in upper layers before the lower ones are complete. The mechanism for improved layerwise growth is oxide formation at the interface, producing a large amount of small islands that encourage interlayer mass transport. The growth of Sm on Mo (110) is generally more rough than Gd on Mo(110) due to the dynamic size change associated with the coordination induced valence transition for the Sm atoms.