The Group on Active Tectonics (GAT) and the Environmental Geophysics University Laboratory (LUGA) at the National Autonomous University of Mexico (UNAM), Campus Morelia seeks applicants for a Postdoctoral Research position. The candidate will pursue fundamental and applied research into either a) active tectonics and/or b) tsunami deposits and paleoseismology with focus on the Mexican Subduction Zone. The candidate will be responsible for the development and execution of field and laboratory research, and to conduct studies on the geologic signature left by great earthquakes and their tsunamis. The fields of application include earthquake hazard, tsunami hazard and long-term earthquake record of this active margin.
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A very nice animation of the 2011 worldwide seismicity for earthquakes M ≥ 4.5 in the following link http://www.youtube.com/watch?v=cwWn_W6ZbT4&feature=youtu.be (with sound intensity for each earthquake plotted on an orthographic globe map).
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Since ten days I am in Greece now with a dozen of students. We started with an excursion in the western Peloponessus area and had a look at the regional tectonics, sedimentology (mainly Neogene Flysch units and young beach rocks), the large limestone horsts of Gavrovo and Ionian units, Ancient Olympia and recent mass movements. Then we began with field work for BSc, MSc and PhD theses. more
The Crestone Science Center (Crestone, Colorado, USA) will be teaching its
annual summer Field Course on Neotectonics and Paleoseismology from May 21
to May 30, 2012, in Crestone, Colorado. This course has been taught since
2001 by James P. McCalpin, editor of the book Paleoseismology (1996, 2009).
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The 2nd INQUA- IGCP 567 International Workshop on “Active Tectonics, Earthquake Geology, Archaeology and Engineering” was held in Corinth 19-24 September 2011. The event has been organized jointly by the INQUA-TERPRO Focus Area on Paleoseismology and Active Tectonics and the IGCP-567 “Earthquake Archaeology”.
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Folks at Arizona State University and San Diego State University are conducting a study to test the repeatability, accuracy, and precision of lateral displacement measurements derived from high-resolution topographic Light Detection and Ranging (LiDAR) data. Please take a few minutes to participate! If you have any questions about the research or would like to use the materials as a classroom exercise, please feel free to email Barrett at jbsalisb@asu.edu.
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The Spanish IGME (Instituto Geológico y Minero de España) has published a great tool for anyone interested in neotectonics and paleoseismology of the Iberian Peninsula. Besides the earthquake catalogues, they have created a GoogleMaps-based database of active faults in Spain and Portugal. more
Dear fellows,
please stop littering the beaches all over the world. Seriously. I like beaches and I guess so do you, so please, take your trash with you. Last week I’ve been to Oman and worked in the Al Sawadi area, where you have a great coast line (which will be spoiled by a huge hotel-apartment-something complex, soon). The only thing was, you almost couldn’t see the sand because it was covered with oil cans, plastic bags, bottles, tires, more oil cans, buckets, toilets (!), packaging shit, cups, and oil cans. Please, stop that.
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Klaus, Ben, Sascha and me went to visit our colleague Gösta at the GUtech in the Sultanate of Oman. We did some fieldwork for our project which deals with coastal changes. Parts of the Omani coast subside, others appear to be stable or are even uplifted. This might be due to large scaled crustal movements (the Makran Subduction zone is nearby) and/or regional effects. We are trying to find good proxies for reconstructing the Holocene sealevel and climate changes. Additionally, we need to get a grip on the neotectonics that affect the coastal areas. more
A very interesting paper by Oskin et al. (2012) published in Science (http://www.sciencemag.org/content/335/6069/702.full) a few days ago shows how the M 7.2 Mexico earthquake in April, 2010, has changed the landscape down to a few cm. The El Mayor–Cucapah earthquake produced a 120-kilometer-long multifault rupture through northernmost Baja California, Mexico. more
