Seismic data of a rockslide: Evaluation of noise levels, site effects, frequency content and identification of seismic phases.

Seismic data can provide information to deduce the occurrence of mass movement events, their release time, event location and dynamics characterization [1]. Nevertheless, the effect of local site amplifications, the level of seismic noise and the frequency content of the signals are important constraints to correctly identify and describe these types of events. In this article we provide data on: site effects, power spectral densities, polarization particle motion and spectrograms generated by a rockslide (∼450 m) (hereinafter NR) recorded in two permanent seismic stations (EPOB and POBL) located ∼10 km from the source.