The discrete wavelet transform (DWT) is currently being used for seismic-ev
ent detection and classification in the New England region. The DWT forms a
new basis set for picking out, from a data stream, important features of a
seismic event: time, energy, and predominant period of the first, peak, an
d last wave-forms. Classification of these events from their features into
one of the following classes, teleseisms, regional earthquakes, near earthq
uakes, quarry blasts, and false triggers, is accomplished with conditional
class densities derived from training data. This algorithm is tested for de
tection and classification performance on the New England Seismic Network (
NESN) of Weston Observatory of Boston College. This detection algorithm exh
ibits a likelihood of detection two times greater than STA/LTA under typica
l wideband network constraints in arbitrary conditions at NESN stations. Cl
assification of seismic events via this method achieves an approximately 70
% correct identification rate relative to a human viewer over a broad range
of data test sets.