In order to propose methodological solutions for reducing seismic risk in Caribbean urban zones, efforts concentrate on applying research activities. For example, elaborating seismic risk scenarios allows a better assessment of the consequences of an earthquake affecting the organization of social structures, in order to highlight sensitive sectors where considering seismic risk must be given priority. Because of its primary objectives, the SYSMIN II program in Dominican Republic takes place in this context. In this paper, we show how methodologies developed during seismic microzonation studies in the French West Indies, were suitable to be applied to the case of Hispaniola, the second island in the Greater Antilles. The north of Hispaniola is threatened by the eventual rupture of a major seismogenic fault zone, named Septentrional. The town of Santiago de los Caballeros in the Dominican Republic is particularly exposed because of its close location to this fault (<10 km). The paper gathers results obtained from the seismic hazard and microzonation studies developed in the city of Santiago: i) quantification of regional seismic hazard dominated by the Septentrional fault, ii) a new geological mapping of superficial formations at the scale 1:10.000, and iii) mapping of zones of homogeneous seismic response and liquefaction susceptibility. These interpretations are based on field geotechnical and geophysical measures, but also on the geological expertise achieved over several years in the Cibao region by the consortium IGME-BRGM-INYPSA. On the French West Indies, the volcanic origin of the geological formations punctuated by sedimentary episodes, gives a particular signature to the amplification phenomena of seismic vibrations due to site effects. The investigations carried out in Santiago revealed a new issue: surprisingly minor site effects (based on the H/V method of ambient noise) in the plastic continental argillaceous unit that represents the main layer for foundations in the whole city area.
Tras el terremoto de Haití de 2010 dio comienzo una iniciativa para estudiar los posibles efectos de los terremotos en la ciudad de Santiago de los Caballeros (República Dominicana); la segunda ciudad más importante del país y que ya fue reconstruida y reubicada en 1562. El daño debido a un terremoto ocurre asociado a un conjunto de factores, entre ellos, la aceleración del suelo. El efecto de la atenuación de la distancia en un radio de unos pocos kilómetros suele ser mucho menos relevante que el efecto de la variación en las propiedades de los suelos. Este artículo recoge los resultados obtenidos de los estudios de peligro sísmico y microzonificación sísmica en la ciudad de Santiago de los Caballeros: i) cuantificación del peligro sísmico regional debido a la falla septentrional; ii) un nuevo mapa geológico y iii) la cartografía de zonas de respuesta sísmica homogénea y susceptibilidad a la licuefacción.
This paper analyses the performance of SAR-based results to support emergency management operations during the volcanic crisis of La Palma island. Tajogaite eruption began on September 19th 2021 affecting a high populated area and the surrounding farmland, used for different agricultural purposes. SAR datasets obtained from Sentinel-1, COSMO-SkyMED, PAZ-TerraSAR-X and Capella satellites, were processed to calculate amplitude, coherence and differential interferograms. These results have permitted to map the morphology of the volcanic cone, the evolution of lava flows and the regional displacements. The comparison of the results obtained with the different satellites has been useful to understand their performance during an emergency scenario triggered by a volcanic eruption. COSMO-SkyMED has provided the most useful information for the analysis of the cone morphology and the lava flows. Sentinel-1 showed the best performance for regional displacements monitoring, whereas PAZ results was the second best option for all the retrieved products.