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tsunamis are generated by earthquakes, some tsunamis are generated by subaerial gravity flows, which can occur not only in oceans, but also in lakes or rivers. Understanding such tsunami generation is a
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seismological methods that use seismic ambient noise for monitoring and early warning of natural hazards and water resources. With fine temporal resolution (daily or even hourly), these methods provide indicators
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-directed by Jean-Mathieu Nocquet, seismologist and IRD research director. Basic knowledge of seismicity is required for this doctoral research, but the candidate will also be able to draw on the support of a
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, for comparison of hydrothermal fluids composition and spatial variations with structural and seismic context along the Ethiopian rift segments. Industry secondment: 45-8 Energy company. Metz – France (https