The 1906 earthquake microzoning is in agreement with the one resulting from the damages of the 1985 earthquake, with an increase of MSK Medvedev-Sponheuer-Karnik intensities of about 1/4.
La micro zonificación del terremoto de 1906 concuerda con la resultante del terremoto de 1985, con un incremento de 1V4 intensidad MSK Medvedev-Sponheuer-Karnik.