I hope you have reserved some time for reading – here comes plenty of great new material on one of the most interesting tectonic features on earth, the Dead Sea Transform. The Israel Journal of Earth Sciences has published a special issue: The Dead Sea Rift as a natural laboratory for neotectonics and paleoseismology, Volume 58, Number 3 – 4. The papers are an outcome of the 2009 INQUA joint Israel/Jordan fieldtrip with the same name. I was lucky enough to have participated in that field trip. It was for sure one of the best field trips I ever had. more
Klaus and me went to the SSA 2012 annual meeting in San Diego in April. The conference was great and very focussed. I really like that kind of rather small meetings, where almost everything is interesting for me. I saw a lot of interesting posters and great talks and especially liked the paleoseismology and archeoseismology sessions (of course!).
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Dear colleagues,
we’ve just published the first circular for the upcoming 3rd workshop on earthquake geology, paleoseismology and archaeoseismology, Morelia, Mexico, 19-24 November 2012. Learn about the scientific program, the meeting program, costs and deadlines, the venue and organizers.
Download the flyer here (3 mb, pdf)!
The 3rd INQUA-IGCP 567 International Workshop on Active Tectonics, Paleoseismology and Archeoseismology will be held in Morelia (Mexico) from 18 – 24 November 2012. The workshop is the continuation of the BaeloClaudia2009 and Corinth2011 events. We invite all scientists in the fields of earthquake geology, paleoseismology, archeoseismology, tsunami studies, earthquake engineering, seismic hazard assessment to participate in the workshop. We will try to provide travel grants from INQUA and IGCP for young scientists. See Acambay1912.org for detailled information, registration and abstract submission.
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Delphi is one of the most impressive places I’ve ever seen. The landscape is just breathtaking – the archaeological site is situated on the southern flank of the Parnassus Mountains, dominating the entire valley. You can see the Gulf of Corinth right from the temples, and due to the steep slope you feel like Delphi is built on many floors with the stadium being the roof. The oracle might be related to faults under the temple; some authors speculate that gas vents (ethane?) caused hallucinations of the priest, which were interpreted as the oracle. Another nice thing is that you can see the archaeoseismological damage from strong historical earthquakes everywhere – cracks, rotated and tilted walls, corner break-outs, dropped keystones in arches and so on. more
The University of Cologne (Seismological Station Bensberg) invites applications for an open position as a Doctoral Student. An essential part of the research activities of the candidate will be dedicated to his/her work on a dissertation project. This work will be part of a research project on Archaeoseismological Studies in Midea and Tiryns, Greece concerned with the possible seismogenic cause of the decline of the great Mycenaean palaces of the Argolis.
Dear colleagues,
We would like to bring your attention to a special session at the 2012 Annual Meeting of the Seismological Society of America (17-19 April, 2012, San Diego, California):”Earthquakes and Tsunamis at Coastal Archaeological Sites”.
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Dear colleagues,
We would like to bring your attention to a special session at the 2012 Annual Meeting of the Seismological Society of America (17-19 April, 2012, San Diego, California): “Macroseismic Effects in Recent and Ancient Earthquakes and their Relationship to Ground Motion Parameters”. more
9:00 The second day started with a great keynote, Chris Scholz talked about earthquake triggering and fault synchronization with examples from California and Iceland.
09:45 Next great keynote: Clark Burchfiel on the Wenchuan EQ!
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After the very successful 1st Workshop on Earthquake Archaeology and Paleoseismology held in the ancient roman site of Baelo Claudia (Spain, 2009), the INQUA Focus Group on Paleoseismology and Active Tectonics decided to elaborate a bi-annual calendar to support this joint initiative with the IGCP-567 “Earthquake Archaeology”. This second joint meeting moved to the eastern Mediterranean, a tectonically active setting within the Africa-Eurasia collision zone and located in the origins of the pioneer’s works on archaeoseismology. However, for the coming year 2012, at least a part of us will move also to the New World, where the 3rd INQUA-IGCP 567 international workshop will take place in Morelia, Mexico in November 2012. It is planned to proceed with the meeting, so we are thinking of Aachen, Germany, to be the host in 2013, possibly together with Louvain, Belgium.
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