We have investigated the homoepitaxial growth of Ag(110) in the multilayer
regime. After deposition of 30 monolayers of Ag at a temperature of 210 K a
ripplelike surface instability is produced and the ridges of the ripples,
as well as the majority steps, are found to be parallel to (1 (1) over bar
0) which is the thermodynamically favored orientation. As the deposition te
mperature is decreased to 130 K, an unexpected 90 degrees switch of the rip
ple orientation is observed. The ridges of the ripples and the steps are in
this case parallel to (100). In the intermediate temperature range a check
erboard of rectangular mounds results. We interpret our results in terms of
the peculiar hierarchy of interlayer and intralayer diffusion barriers pre
sent on the anisotropic Ag(110) surface.