Wetting or dewetting on soft elastomeric surfaces is largely controlled by
the dissipative properties (viscoelasticity) of the substrate. The componen
t of liquid surface tension acting perpendicularly to the solid causes a de
formation, or "wetting ridge", which must be displaced with the triple line
. Previously, triple line motion due to capillary imbalance has been studie
d, whereas in the present work, we consider liquid motion due to gravity. L
iquid drops running down an elastomeric plane move at a speed largely deter
mined by the properties of the polymer. Results obtained agree well with th
e theory and demonstrate how motion depends on the state of the polymer, th
e angle of inclination of the plane, and drop volume.