Evidence is presented for the origin of high-resistivity barriers at c
ertain interfaces in high-field varistor materials. The barriers give
rise to terrace contrast which can be observed using remote electron b
eam induced current imaging in the SEM. It is proposed that these inte
rfaces, which are often associated with a thick intergranular layer of
a compositionally distinct bismuth rich oxide, are relicts of the pow
der structure and correspond to agglomerate surfaces. It is suggested
that the presence of these resistive surfaces ultimately limits the cu
rrent that can flow at breakdown.