For Tb(0001), a surface core-level shift of the 4f7 photoemission mult
iplet of delta(s)=0.26+/-0.03 eV is determined. This value is by more
than a factor of 2 smaller than the result of a recent self-consistent
SLAB calculation, but agrees with the prediction of a thermochemical
model. It is demonstrated that the larger values of delta(s) reported
previously for polycrystalline samples originate from contributions of
low-coordinated surface sites. Implications of the present findings f
or an improved understanding of the surface electronic structure of ra
re-earth metals are briefly discussed.