The Journal of Iberian Geology has now published a Special Issue “Active Faults in Iberia“, with J.J. Martínez-Diaz, E. Masana, and M.A. Rodríguez-Pascua as guest editors: J Iber Geol, 38 (1), 201. This volume comprises a great collection of new data on active faults, paleoseismology, intraplate earthquakes, and seismic hazard. One article also introduces the Quaternary Active Faults Database of Iberia. And the best thing is – all articles are open access and available for download! more
The early bird registration for the Acambay2012 workshop ends on 1 July. Until then, you pay max $190, later it will be up to $250. The 3rd INQUA-IGCP567 International Workshop on Active Tectonics, Paleoseismology and Archaeoseismology takes place in Morelia, Mexico, from 19 – 24 November 2012. It is held due to the 100th anniversary of the Acambay earthquake (1912). Check the workshop website for more information, this will be a great meeting, I am sure, so I will go there. more
Our colleagues from the Bulgarian Academy of Science, Geological Institute “Strashimir Dimitrov“, have published a report on the coseismic and secondary effects of the May 22, 2012 Pernik earthquake, Western Bulgaria. The earthquake had a magnitude of MW5.6, see this special website of EMSC. Radulov et al. report intensities of up to VII (MSK) and various coseismic and secondary earthquake effects. more
Today is GeoScience Day (Geotag) at RWTH Aachen University! Organized by the Chair of Engineering Geology and Hydrogeology, this event will start at 9:30 am in the Couvenhalle, Aachen. Geoscience-related talks and a poster exhibition will only be some parts of the very interesting program. The Geo summer party will be started after the “Geotag” at 6:00 pm at the parking lot of the Geoscience Institute at Wüllnerstraße. Come and see! Follow the Geotag on Twitter (hashtag #GEOTAG) and Facebook, and visit the official website! more
The Gulf Stream is ensuring the mild climate in Europe, everyone knows that. But does it really? Read Chris Rowan’s article on climate, Gulf Stream, heat capacity and atmospheric circulations.
Ritz et al. published a paper on the paleoseismicity of the North Tehran Fault, Iran. From trenching studies they claim at least 6 surface-rupturing events during the last 30 ka. Read the paper here at JGR-Solid Earth. Ritz, J.-F., H. Nazari, S. Balescu, M. Lamothe, R. Salamati, A. Ghassemi, A. Shafei, M. Ghorashi, and A. Saidi, 2012: Paleoearthquakes of the past 30,000 years along the North Tehran Fault (Iran), J. Geophys. Res., 117, B06305, doi:10.1029/2012JB009147. more
One of the best blog articles I recently read deals with the problems scientists face when they are interested in public outreach. Scicurious perfectly summarizes our situation.
The transit of Venus was a spectacular event, unfortunately not visible from Aachen. A really great photo collection is here at The Big Picture (Boston.com). A cold comfort for those who missed it (like me). They always have the best pictures there, by the way. more
Three papers published recently caught my eyes. First, Andrej Gosar investigated the earthquake environmental effects (EEEs) of the 12 April 1998 Mw =5.6 Krn Mountains earthquake, Slovenia. The quake measured VII-VIII on the EMS-98 scale, and Andrej found that the intensities reached the same values on the ESI2007 scale. He reports that the intensity distributions for both scales are comparable, but show some differences due to the sparsely populated epicentral area. The research concentrated on rockfalls for EEE determination. It’s a nice example that also moderate events can be characterized using the ESI2007 scale.
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More than two weeks have gone now after the Mw6.1 earthquake in Northern Italy, and a very strong aftershock has rattled the area again and caused casualties and more buildings to collapse. Several reports are already published on that event and we have lots of data which is waiting to be analyzed. Here’s a summary of data sources: more
The University Insubria (Como, Italy) has published the first report on the earthquake environmental effects that accompanied the Northern Italy “Finale Emilia Earthquake” of 20 May, 2012. On that day, a quake with magnitude Mw6.1 rocked the Po Plain, leaving seven people dead and hundreds of houses damaged. On 29 May, a very strong M5.8 aftershock occurred in the region. more
The INGV has published some new data on the earthquake that hit Italy in the morning of 20 May, 2012 and caused damages and casualties. Peak ground accelerations (PGA) reached 28%g in the epicentral area. This is not unusual for an event of that size. Peak ground velocities (PGV) were as high as 20 cm/s. The spectral response is more interesting. The 3s period response is 1.5%g only, at 1s period the area encountered 18%g, and for the 0.3s period the values reached 49%g, which is quite a lot for a Mw6.1 quake. However, the longer periods tend to be more dangerous for buildings. more
