Prof.
Klaus-G. Hinzen
(Cologne University)
10/25/18, 11:00 AM
Keynote
Earthquakes cause ground motions and ground motions can cause damage to engineered structures. Engineering seismology’s main goal is to design structures that withstand such ground motions. Models for simulating ground motions, given that the seismic source and the travel path parameters can be assumed or are known, can be constructed which can help quantify damage scenarios. By applying a...
Dr
Silke Beinersdorf
(Dr.-Ing.)
10/25/18, 11:40 AM
Session 3 Orals
Oral Preference
The completion of version 2.1 of the magnitude-oriented earthquake catalogue for German and adjacent areas EKDAG - extended Ahorner catalogue (as of December 2014) gave rise to the question of the influence of current catalogue entries (or their changes) and the hazard analyses highlighting them on practical engineering applications. This question was fundamentally extended to the question of...
Mr
Miklos Kazmer
(Eotvos University)
10/25/18, 12:00 PM
Session 3 Orals
Oral Preference
There is more in archaeoseismology than just a good story - wrote Manuel Sintubin and co-authors back in 2008 (SRL 79). Observations abound, get published, interpreted and various conclusions are drawn, more or less well-founded. However, due to the nature of excavations and restorations valuable information is lost if not documented properly and in time. Much information is lost due to the...
Dr
Hélène Dessales
(Ecole normale supérieure)
10/25/18, 1:00 PM
Keynote
Due to its particular geological context, the town of Pompeii and its surroundings are an exceptional ‘laboratory’, subject to a double volcanic and seismic risk. It stands out as it wasthe victim of two earthquakes before the eruption of Vesuvius in 79 AD. The first, in 63 AD is well known because it is recorded in the texts of Seneca and Tacitus, while the second, which happened around the...
Laurence Audin
(ISTerre France)
10/25/18, 1:40 PM
Oral Preference
In South America, human beings are prone to settle along fault scarps. Emblematic among them in Peru, the touristic and tectonic Cuzco region is affected by damaging earthquakes since the Spaniards arrived, as demonstrated by the 1650, 1950 and 1985 events. This area in the high Altiplano, sitting 400km away from the subduction zone, exhibits a combination of strong seismic hazard and high...
