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Evento Fecha Hora(GMT)* Latitud Longitud Prof.(km) Int. Máx. Mag. Tipo Mag. (**) Localización
1201326 27/03/2013 16:10:55 27.7759 -18.2395 10 4.4 4 W FRONTERA.IH
At distant seismograph stations, the pP follows the P wave by a time interval that changes slowly with distance but rapidly with depth. This time interval, pP-P (pP minus P), is used to compute depth-of-focus tables. Using the time difference of pP-P as read from the seismogram and the distance between the epicenter and the seismograph station, the depth of the earthquake can be determined from published travel-time curves or depth tables.
Originally posted by Olivine
reply to post by rigel4
Thanks rigel4.
TA's thread concerns a different Canary Island, La Palma, and possible harmonic tremor associated with the Cumbre Vieja volcano.
My thread is covering the earthquakes occurring toward the west end of El Hierro, which, as of yet, do not show any harmonic tremor, but are volcano related.edit on 3/27/2013 by Olivine because: (no reason given)
La no existencia de datos sobre este parámetro durante los periodos de tiempo enlazados por lineas discontinuas se debe a la carencia de recursos para haber mantenido una presencia permanente del INVOLCAN en El Hierro desde el pasado mes de abril de 2012.
The lack of data on this parameter during the time periods linked by broken lines is due to the lack of resources to have maintained a permanent presence Involcan in El Hierro since last April 2012.
Evento Fecha Hora(GMT)* Latitud Longitud Prof.
(km) Int. Máx. Mag. Tipo Mag. (**) Localización
1202124 29/03/2013 17:01:21 27.7309 -18.3148 20 Sentido 4.7 4 ATLÁNTICO-CANARIAS