The great Lisbon earthquake of November 1st, 1755 with an estimated moment magnitude
of 8.5–9.0 was the most destructive earthquake in European history. The associated tsunami …

This work presents a macroseismic analysis of the AD 1755 Lisbon Earthquake-Tsunami
event by means of the combination of intensity data derived from the EMS-98 scale and the …

In the study of palaeotsunamis it is crucial to decipher the sedimentological record, to derive
intensity of past events and to infer different inundation phases. To achieve this goal, it is …

An earthquake early warning system (EEWS) can provide valuable alerts before the
destructive seismic waves arrive. This warning time can allow the adoption of protective …

Preventive management strategies are evolving towards multi-hazard risk estimates.
Commonly, the multi-hazard characterization is pursued following a probabilistic approach …

Seismicity along the western part of the Eurasia–Nubia plate boundary displays very
complex patterns. The average motion is transtensional in the Azores, dextral along the …

Deepwater landslides are often underestimated as potential tsunami triggers. The North
Gorringe avalanche (NGA) is a large (∼ 80 km3 and 35 km runout) newly discovered and …

In probabilistic seismic‐hazard analysis (PSHA), seismic source zone (SSZ) models are
widely used to account for the contribution to the hazard from earthquakes not directly …

A geodatabase of landslides and other geomorphologic and hydrologic phenomena,
triggered by earthquakes in Portugal, was built based on the analysis of historical records …

Portugal, located in the southwest region of the Eurasian plate, has been affected by several
destructive earthquakes throughout its history, the most well‐known being the 1755 Great …