From its launch in October 1989 until the end of 1992, the Galileo spa
cecraft traversed interplanetary space from Venus to the asteroid belt
and successfully executed close flybys of Venus, the Earth, and the a
steroid Gaspra. The dust instrument has been operating most of the tim
e since it was switched on in December 1989. Except for short time int
ervals near Earth, data from the instrument were received via occasion
al(once per week to once per month) memory read outs containing 282-81
8 bytes of data. All events (impacts or noise events) were classified
by an onboard program into 24 categories. Over the three-year time spa
n, the dust detector recorded 469 ''big'' dust impacts. These were cou
nted in 21 of the 24 event categories. The three remaining categories
of very low amplitude events contain mostly noise events. The impact r
ate varied from 0.2 to 2 impacts per day depending on heliocentric dis
tance and direction of spacecraft motion with respect to the interplan
etary dust cloud. Because the average data transmission rate was very
low, some data were not received on the ground. Complete data sets for
358 ''big'' impacts were received, but the other 111 ''big'' impacts
were only counted. The observed impact rates are compared with a model
of the meteoroid complex.