[1] Some alternative representations for seismicity are introduced based on
the use of the hue, saturation, and brightness model of color representati
on. Depth information is conveniently coded by hue and magnitude by saturat
ion. The approach can be used for individual events or to provide useful su
mmary properties of seismicity. The cumulative effects of many events can b
e combined by converting body wave magnitude into an equivalent energy or s
train release and then summing the energy or strain contributions in a part
icular cell, finally converting back to an effective magnitude over a 10-ye
ar period for plotting. Time averaging improves the reliability of the info
rmation and can provide a clearer picture of the balance between seismic ev
ents at different depths.