This paper describes a study of the resonance phenomenon of a 2-D allu
vial valley embedded in a half-space and subjected to an incident plan
e SH wave. The scattered wave and refracted wave are expressed as a se
ries of basis functions, and both the scattered and refracted coeffici
ents can be related to the incident wave by the so-called T-matrix met
hod. By using singular-value decomposition and solving the eigenvalue
problem, one can decouple the effects of all resonance modes. Therefor
e, the amplification factor of each partial eigenwave can be found, an
d used to determine the resonance frequencies of each normal mode and
its overtones. The motion of the ground subjected to the incident plan
e SH wave and the mode shape of each single normal mode are determined
and discussed for semicircular and semi-elliptical alluvial valleys.