Seismic signals generated by artificially released avalanches were studied
from the seismological viewpoint in the time and frequency domains in an at
tempt to characterise them for monitoring purposes. The avalanches were art
ificially released and the corresponding seismic signals were recorded at d
ifferent sites within a radius of up to 3 km together with the video images
with a common time reference. The results obtained indicate that avalanche
s following the same path and recorded at the same site present similar sei
smic signals. A relationship between the avalanche seismic signals (amplitu
de, frequency content and wave trains) and the avalanche path was observed.
The sources of the recorded seismic signals corresponds to avalanche path
slope changes, interaction with obstacles and phenomena associated with the
stopping stage of the avalanche. Local site effects were also present. The
se results lend support to the use of seismic signals as an efficient metho
d of monitoring areas where avalanches are frequent and human observation i
s difficult. (C) 2000 Elsevier Science Ltd. All rights reserved.