An initial empiric fractal based model for the breakage of rock has be
en outlined, which was based on the single impact failure of single co
res of rock. This incorporates the variance of specific impact energy,
and to some degree the starting size, upon the resultant breakage pro
ducts. The important parameter of interest is the fragmentation fracta
l dimension which represents the power-law size-frequency distribution
of the progeny, and is in essence a measure of the degree of fineness
of the population. This quantity possesses a theoretical basis and of
fers an alternative approach for studying comminution events. As the a
pplication of fractal geometry has become more widespread the associat
ed terminology has been widely adopted, but it can sometimes represent
a pointless shift in vocabulary. This is particularly the case with p
ower-law relationships that do not directly relate to a physical struc
ture. In the situation described here the notation is justified as the
fragmentation fractal can be derived directly from fractal theory, an
d is fundamentally associated with the coastline or boundary fractal d
imension of the particles within the distribution. Copyright (C) 1996
Elsevier Science Ltd