Bibcode
Berrocoso, M.; Fernandez-Ros, A.; Prates, G.; Martin, M.; Hurtado, R.; Pereda, J.; Garcia, M. J.; Garcia-Cañada, L.; Ortiz, R.; Garcia, A.
Bibliographical reference
EGU General Assembly 2012, held 22-27 April, 2012 in Vienna, Austria., p.4351
Advertised on:
4
2012
Citations
0
Refereed citations
0
Description
The surface deformation has been an essential parameter for the onset
and evolution of the eruptive process of the island of El Hierro
(October 2011) as well as for forecasting changes in seismic and
volcanic activity during the crisis period. From GNSS-GPS observations
the reactivation is early detected by analizing the change in the
deformation of the El Hierro Island regional geodynamics. It is found
that the surface deformation changes are detected before the occurrence
of seismic activity using the station FRON (GRAFCAN). The evolution of
the process has been studied by the analysis of time series of
topocentric coordinates and the variation of the distance between
stations on the island of El Hierro (GRAFCAN station;IGN network; and
UCA-CSIC points) and LPAL-IGS station on the island of La Palma. In this
work the main methodologies and their results are shown: •The
location (and its changes) of the litospheric pressure source obtained
by applying the Mogi model. •Kalman filtering technique for high
frequency time series, used to make the forecasts issued for volcanic
emergency management. •Correlations between deformation of the
different GPS stations and their relationship with seismovolcanic
settings.