VLF plasma wave measurements obtained from the Pioneer Venus Orbiter E
lectric Field Detector (OEFD) have been used to construct statistical
images of the Venus foreshock. Our data set contains all upstream meas
urements from an entire Venus year (approximately 200 orbits). Since t
he foreshock VLF characteristics vary with IMF orientation we restrict
the study to IMF orientations near the nominal Parker spiral angle (2
5-degrees to 45-degrees). Our results show a strong decrease in 30 kHz
wave intensity with both foreshock depth and distance. There is also
an asymmetry in the 30 kHz emissions from the upstream and downstream
foreshocks. The ion foreshock is characterized by strong emissions in
the 5.4 kHz OEFD channel which are positioned much deeper in the fores
hock than expected from terrestrial observations. No activity is obser
ved in the region where field aligned ion distributions are expected.
ULF wave activity, while weaker than at Earth, shows similar behavior
and may indicate the presence of similar ion distributions.