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Co-seismic surface structures

In the first discussion with the local authorities and our guide, we also talked about the effects and damages of the El Galpón earthquake. The damages in the village were obvious and I wrote about them in the last post. But for us seismologists it is also interesting to see if there are damages in the landscape. Typical effects would be: cracks in the ground, landslides, water and sand fountains, a new step in the topography or changes in the ground water table. We call this stuff co-seismic effects, because they occur during the shaking of an earthquake. Some of these (i.e. changes in the ground water table) can occur before an event as pre-seismic or after an event as post-seismic events (e.g. landslides).
Luckily, the people understood what we were pointing at and they showed us pictures of big cracks in the ground. They found them directly after the earthquake, so they could be our co-seismic effects. On our last day of fieldwork we had some time left to have a look on these cracks in the ground. Read More…


The damages in El Galpón

During our fieldwork we had the chance to visit the village El Galpón, which was mainly affected by the earthquake in October 2015. To give a visible expression how much shaking can be generated by a 5.7 Mw earthquake watch this video of a security camera in the city of Metán, approximately 50 km away from the epicenter.

El Galpón is quite small and only has some hundreds inhabitants. When we first arrived we thought the people removed the damages really quick or nothing really happened. When we got closer to the center we investigated the latter was true. The newer buildings in the outer part had no obvious damage. But in the central part most of the buildings were stabilized by wooden planks.

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The necessity of local networking

This post is a preparation for the summary of the last week of our fieldwork in Argentina. In addition, it’s a big thank you to our locals who helped us a lot and made the work that successful as it was. Read More…

fieldwork in the jungle

The reason for the first visit of Argentina is the field-school organized within our StRATEGy program. This field trip is about 10 days only and we thought it would be a good idea to prolong the stay a few more days and get an impression of the area and search for possible sites for our seismographs. Hence, my second PI Gela and me left Germany 4 days earlier and teemed up with the Argentinian Professor Antonio and his student Ahmad to explore the Candelaria range 150km north of Tucumán.

Unfortunately, March is the end of the monsoon season; we got already surprised when we arrived in Tucumán by a typical convective rainstorm which lasted only 10-15 minutes, but enough time to flood all streets and sidewalks. Also the landscape responded to these weather conditions and I want to explain in this post how everything was affected.

I may should add that in this region you have 500-700 mm of precipitation during the year, but it will mainly happen in the summer monsoon. But due to El Niño this year, it is a lot more rainfall this summer. Read More…