Sympathetic nucleation is defined as the nucleation of a precipitate c
rystal at an interphase boundary of a crystal of the same phase when t
hese crystals differ in composition from their matrix phase throughout
the transformation process. Following a brief history of the discover
y and interpretation of this phenomenon, the means of identifying the
presence of sympathetic nucleation are described. The morphological co
nfigurations most frequently produced by sympathetic nucleation are il
lustrated. Heterogeneous nucleation theory is then applied to explain
sympathetic nucleation. Particular emphasis is placed upon the driving
force for sympathetic nucleation, since many of the effects of phase
diagram geometry and supersaturation upon sympathetic nucleation can b
e simply explained upon this basis.