Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/13128
Authors: Rodriguez, Luz M.* 
Sarabia, Ana M* 
Perez, Carol* 
Mora, Héctor* 
Singer, André* 
Salcedo, Elkin* 
Yepez, Santiago* 
Cifuentes, Hernán* 
Diederix, Hans* 
Torres, Eliana* 
Rodriguez, José A* 
Aufemard, Franck* 
Gómez Capera, Augusto Antonio* 
Leal, Alejandra* 
Title: Inventario de Daños y Efectos Geológicos Co y/o Post-Sísmicos del Sismo Ocurrido el 18 de mayo de 1875, en la Frontera entre Colombia y Venezuela
Journal: Revista de la Academia Nacional de la Ingeniería y el Hábitat 
Series/Report no.: /30(2015)
Issue Date: Sep-2015
Keywords: historical seismicity
destruction of communities
Subject ClassificationSeismology
Abstract: On the border between Colombia and Venezuela, have occurred seismic events with important records of damage in both countries. In this paper, we study the historical earthquake that took place on May 18, 1875 between 11.15 and 11.30 in the morning (the time was the same for communities in both countries since there was no time zone difference), which is catalogued as a border earthquake due to the report of damages in the cities of both nations. The community of San José de Cúcuta, current capital of the Northern State of Santander, Colombia, registered the greatest number of deaths and damage to buildings. An inventory of the geological damage and co -seismic and postseismic effects was created based on information of previous studies and data obtained from archival primary sources from Colombia and Venezuela. The result is a bi-national database, which includes the summaries of historical descriptions with the effects in the persons and objects, the geological damages and effects observed during the seismic event. These data has led to the creation of a table of MM and EMS-98 intensities, which enables the identification and delimitation of the regions of greater damages. The maximum level intensity is I=10 in the cities of San José de Cúcuta, Villa del Rosario, Pueblo de Cúcuta (San Luis) in Colombia and San Antonio, San Juan de Ureña in Venezuela. Moreover, we formulated a table of intensities using the ESI-2007 INQUA scale, based on the information of geological observations described in historical documents. These data are related to the epicentral zone with an approximate radius of 30 km.
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