Posts in the category »   «  ( 123 Posts )

  • Paleoseismology Through Sedimentology

    The Megablock Complex: An example from the East African Rift

    Recognizing and interpreting seismite horizons (soft-sediment deformation generated by earthquakes) preserved in the sedimentary record is an underappreciated approach for paleoseismic analysis. The addition of sedimentological studies to a toolkit that includes other well-established methods, such as instrumental seismic monitoring and fault trenching, can provide a less expensive and more practical option for earthquake hazard prediction and preparation in certain areas. For example, this may be a good option in less developed regions and in areas where fault trenching may not be possible. Moreover, there is a lot that we can learn rheologically from the study of seismites that could be invaluable for modeling the behavior of the surface/near-surface during seismic activity. Similarly, investigating Quaternary strata in areas that may be prone to seismicity, which may or may not have a recorded history of major earthquakes, can illuminate important information about earthquake recurrence patterns and intervals, in much the same way as fault trenching. more

  • An update on paleoseismology literature

    Here are my latest updates on papers and books that deal with paleoseismology, active tectonics, tsunamis and similar topics. There is a good portion of lake/turbidite paleoseismology with some beautiful seismites. We also have some more general tectonics/review papers, and an interesting attempt to establish a global fault database. Plus, there is an intense ongoing discussion about Kashmir and news from Napa. Enjoy!

    You feel there’s something missing? Drop me a mail!

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  • ISPRA volume “Earthquake Environmental Effect for seismic hazard assessment: the ESI intensity scale and the EEE Catalogue”

    Earthquake Environmental Effects (EEE) have proven to be valuable for describing past earthquakes and their geological imprints. The ESI2007 is a relatively new intensity scale dedicated to such effects, but also integrating traditional macroseismic scales. Examples of ESI2007 intensities assigned to large earthquakes are being collected in the EEE web catalogue hosted by the ISPRA and ESI2007-related work is conducted in the framework of INQUA.

    Another milestone now has been achieved with the ISPRA volume “Earthquake Environmental Effect for seismic hazard assessment: the ESI intensity scale and the EEE Catalogue”. This book is now available online here. It contains updates on the ESI2007, examples of applications, documentation of the EEE Android App, a huge reference list and, most importantly, the ESI2007 description in ten languages: more

  • New paleoseismology literature

    It was quite a long break since I’ve posted the last literature round-up and that’s why the list is really long today.  Here are the latest papers on paleoseismology, active tectonics, archaeoseismology and (paleo-)tsunamis. more

  • This was the Fucino15 meeting – part III

    In the last two posts I have reported on the scientific sessions of the Fucino15 conference and on the first of the field trips. This post is about the L’Aquila field trip. I haven’t been to this city before and I was curious to see the place that sadly became so famous in earthquake science. I was surprised by how many heavily damaged buildings were still standing and by the overwhelming amount of historical buildings that await their reconstruction. We were given a great tour through the Palazzo Ardinghelli which is currently being rebuilt, then we had a look at the worst-affected parts of the city. Here’s a report in images. more

  • This was the Fucino15 meeting – part II

    I blogged about the scientific sessions at the Fucino15 meeting last week, here’s my report about the pre- and post-meeting field trips. The pre-meeting field trip was held in Rome, where we explored the archaeological and historical evidence for earthquake damage in the Eternal City. After the conference we followed the traces of the 1915 Fucino earthquake and then finally visited L’Aquila. This blog covers Rome and the geological field trips, a special on L’Aquila will follow later. more

  • This was the Fucino15 meeting – part I

    Phew, this was an intense week and a great one too! The Fucino15 meeting on paleoseismology, active tectonics and archaeoseismology is over and hopefully everyone safely arrived back home. Here’s a brief report on some of the science that happened at the meeting. Since we had ~50 oral presentations, only an overview is possible here. In the following days I’ll add more details about the field trips. A big thank you to the Italian organizing team who did an amazing job – grazie mille! more

  • What’s up? The Friday links (78)

    Welcome back from all the EGU Vienna, SSA Pasadena and INQUA Fucino meetings during the last days. You have missed a lot of stunning images. Today is Friday and here are your links!

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  • Fucino2015 conference – Program out now!

    The most important paleoseismology event of the year is just a few days ahead and we’re all excited to meet in sunny Italy. The 6th INQUA International Workshop on Active Tectonics Paleoseismology and Archaeoseismology will be held from 19-24 April 2015 in Pescina, Fucino Basin, Italy. The meeting will commemorate the 100th anniversary of the devastating 1915 Fucino earthquake. Make sure to check the final program which is now available for download at the meeting website: download here (PDF, 9 mb).

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  • Submarine Paleoseismology Workshop at ETH Zurich, 16-18 July 2015

    From 16-18 July, 2015, an interesting workshop will be held at ETH Zurich (Switzerland): Submarine Paleoseismology – Using giant piston coring within IODP to fill the gap in long-term records of great earthquakes.

    Michael Strasser, one of the main organizer, names the aims of the workshop: “The main topic of the workshop is to discuss and define a strategy how and where we could best make use of giant piston coring efforts within the Integrated Ocean Discovery Program (IODP) to make some major advancements in submarine paleoseismology to constrain earthquake recurrence beyond historical times.more