This paper outlines the results of the double impact failure of indivi
dual cores of rock, the progeny of which were described by a fragmenta
tion fractal dimension. This, swing pendulum generated, data was compa
red to that previously established from the single impact breakage of
rock cores, and the fragmentation fractal was found to be a suitable t
ool by which the two mechanisms could be assessed. The swing pendulum
data was seen to adequately comply with an empiric based fractal model
of fragmentation derived from the above mentioned single impact tests
. Although an additional consideration was necessary to account for th
e velocity of the impact event, this indicated that the model may have
wider application and be relevant to the impact failure of rock in ge
neral. However, ultrafast load cell testing of selected rocks illustra
ted that a previously postulated function for describing the relation
of fragmentation fractal and size of the parent particle did not hold.
The extrapolated fragmentation fractal significantly under estimated
that directly obtained from the progeny of the ultrafast load cell exp
eriments. (C) 1997 Elsevier Science Ltd.