The effect of viscosity variations associated with large scale chemica
l heterogeneities on mixing in the mantle is studied for a model two-d
imensional problem. Low viscosity regions are rapidly deformed, develo
p long tendrils, and are entrained towards regions of surface divergen
ce. Very viscous regions are only slowly stretched; thus, geochemical
reservoirs can persist relatively undisturbed for long periods of time
if they are > O(10 - 100) times more viscous than the surrounding man
tle. High viscosity ratio blobs have a tendency to aggregate, leading
to the formation of large scale heterogeneities from smaller ones.