Posts in the category »  Earthquake «  ( 116 Posts )

  • Mw4.4 earthquake in the Fucino Basin

    On 28 February, an earthquake of MW4.4 occurred in the Fucino Basin in Central Italy. The event did not cause any damage and was not widely felt. Such an earthquake is nothing special for this area, but it’s interesting because from 19-24 April the 6th INQUA meeting on paleoseismology will be held in Pescina. The conference will bring together scientists from all around the world to discuss latest developments in active tectonics, paleoseismology and similar topics, and its date and location were chosen to commemorate the devastating Fucino earthquake of 1915. This quake left more than 33,000 people dead and was one of the largest earthquakes to hit the Mediterranean in modern history. It was also subject to a number of paleoseismological studies (see links below). more

  • Free book: Catalogue of the geological effects of earthquakes in Spain (in Spanish)

    Spain may not be as famous for its earthquakes as Greece, Turkey or Italy, but significant events do shake the western part of the Mediterranean, too. Numerous paleoseismological and archaeoseismological studies as well as research on historical quakes have been undertaken on the Iberian peninsula. A new book was now published by the IGME which collects all the information currently available on the geological effects of earthquakes in Spain. The book is in Spanish and available for free download here:

    http://www.igme.es/Publicaciones/PubliGratuitas.htm

    The catalogue includes 44 quakes between 218 BC and AD 2011.

    more

  • New report on the Napa Earthquake available, update on amount of afterslip

    Our colleague Tim Dawson from the California Geological Survey (CGS) pointed me to this website, where reports and data on the Napa Earthquake of 24 August, 2014, are collected. There is a new document available for download, the EERI report at the top of the page, which adds some previously unpublished information, especially on the observed afterslip. Tim writes that “afterslip along the central 6-7 km of the rupture is about 35 cm (whereas it was initially only about 20 cm the day of the earthquake).” The afterslip seems to be still ongoing and is monitored with InSAR. more

  • A Double Ethical Bind Along the Dead Sea Fault?

    “Each of us has to decide what the right balance is between being effective and being honest.” 

    I was thinking of this quote whilst listening to Mustapha Meghraoui’s talk during this week’s ISEMG conference in Mugla (Turkey). Mustapha was reviewing the seismic hazard potential of the northern stretch of the Dead Sea Rift, and he ended by identifying two prominent areas where there was a substantial long-term (1000 yr) slip deficit that strongly suggested heightened future earthquake potential. The quote above has nothing to do with earthquakes. Neither is it by Mustapha. Instead, it relates to global warming and was from the climate modeller and policy advocate Stephen Schneider. Nevertheless, it struck me that what Schneider was wrestling with a decade or so ago with climate change has parallels to what some earthquake geologists are wrestling with now: what do we do when we believe that the science demands action? more

  • 3He dating of rockfalls helps to distinguish between proximal and distal paleo-earthquakes in Christchurch, NZ

    The 2011 Christchurch earthquake series had severe consequences and surprised scientists for many reasons. Ground motions were extremely strong despite the relative moderate magnitudes of the quakes (MW 5.3-7.1). The events happened on a system of hitherto unknown faults, some of which are located directly below Christchurch. Earthquake environmental effects (EEE), especially liquefaction, were intense and widespread. It turned out that subsequent quakes reactivated the same feeder dikes of sand blows, showing that saturated sediments are susceptible of liquefaction no matter if they had been liquefied recently (also see the paper of Quigley et al. (2013) on the liquefaction effects). Another stunning lesson was the occurrence of intense rockfall in the vicinity of Christchurch. In a recently published study, Mackey and Quigley (2014) dated rockfall boulders with 3He and show that they allow to estimate the recurrence intervall of local seismic events like the 2011 series. This works is a very interesting way to use EEE for paleo-earthquake studies. more

  • GEER report on the Napa earthquake online

    The M6.0 Napa earthquake came along with some interesting effects. It produced relatively large surface ruptures, but only minor secondary earthquake environmental effects like localized lateral spread, almost no liquefaction and rockfalls, but some hydrological changes. Dozens of geoscientists went out for mapping the earthquake ruptures, supported by InSAR data that precisely show where the ground moved.

    Now the Geotechnical Extreme Events Reconnaissance (GEER) Association published a 400-pages report on their findings. The report is available for download here. Make sure to read it, it’s full of data and great photographs of surface ruptures.

    Other interesting articles and posts on the Napa quake: more

  • New project for inventory and mapping hazardous faults in South America launched

    In 2013 the Global Earthquake Model (GEM) –www.globalquakemodel.org – published seven Requests for Proposal covering topics related to the compilation of basic datasets as well as the creation and calculation of an updated probabilistic seismic hazard input model for South America. This initiative is now named the South America Risk Assessment Project (SARA).

    Five consortia of South American researchers responded to this request and submitted proposals for the Hazard Component of SARA. These proposals has been recently endorsed by GEM and will constitute different datasets or topic layers for SARA. They include databases on historical and instrumental seismicity, hazardous faults (Quaternary deformation), tectonic geodesy and ground motions. more

  • An Indian Ocean tsunami triggered remotely by the onshore M7.7 earthquake in Balochistan, Pakistan, on 2013-09-24

    On 24 September, 2013, a magnitude 7.7 earthquake occurred in Balochistan, Pakistan. The quake caused intense ground motions and had dramatic consequences – hundreds of people died, and more than 100,000 lost their homes. A secondary effect which caught much attention in the international media was the birth of an island off the Pakistani coast – Zalzala Jazeera or Earthquake Island. Another effect which went almost completely unnoticed was a small tsunami in the Arabian Sea. The tsunami reached wave heights of around 1 m at the Omani coast. In a paper which was recently published in Geology, my colleagues and me document the tsunami effects in Oman. We conclude on a submarine slide off Pakistan as the likely trigger mechanism.

    more

  • Paleoseismological field work in Kazakhstan

    During the last three weeks I have been to Kazakhstan for paleoseismological field work and to summarize this journey: It was amazing! The trip was part of the Earthquakes without Frontiers project (EwF). This research project is funded by NERC and ESRC and aims on increasing the knowledge on earthquake hazards in Central Asia. The field work was lead by Richard Walker and scientists from Kazakhstan, Kyrgyzstan, and the UK had a close look at fault scarps in the easternmost parts of the country. Our aim was to determine the slip rates of some of the longest and most prominent thrust and strike-slip faults in the area. more

  • Central European trenching goes on!

    This summer and fall will be trenching time, our Belgian, Dutch and Austrian colleagues are opening paleoseismological trenches. The DEM/image of the last post by Christoph shows already some morphological relevant faults in the Aachen area (recognized by the rectangular open-pit lignite mines) that are striking NW-SE. more

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