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Historical intensity VIII earthquakes along the Rhone valley (Valais, Switzerland): primary and secondary effects

Fritsche, Stefan ; Fäh, Donat ; Schwarz-Zanetti, Gabriela

In: Swiss Journal of Geosciences, 2012, vol. 105, no. 1, p. 1-18

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    Titre
    • Historical intensity VIII earthquakes along the Rhone valley (Valais, Switzerland): primary and secondary effects
    Auteur
    • Fritsche, Stefan. Schweizerischer Erdbebendienst, Sonneggstr. 5, 8092, Zurich, Switzerland
    • Fäh, Donat. Schweizerischer Erdbebendienst, Sonneggstr. 5, 8092, Zurich, Switzerland
    • Schwarz-Zanetti, Gabriela. Schweizerischer Erdbebendienst, Sonneggstr. 5, 8092, Zurich, Switzerland
    Type de document
    • Postprint
    Langue
    • Inglese
    Publié dans
    • Swiss Journal of Geosciences, 2012, vol. 105, no. 1, p. 1-18. SP Birkhäuser Verlag Basel
    Autre version électronique
    Identifiant OAI-PMH
    • oai:doc.rero.ch:316269
    Summary
    In recent years the upper Rhone Valley has been one of the most intensively investigated regions by the Swiss Seismological Service. The high seismicity in the region encourages research in the seismological field and one main focus has been historical seismology. This report presents the state of the art of our historical investigations by giving an overview of the effects of four damaging earthquakes with intensity larger than VII, for which a fairly large number of documents could be found and analyzed. The overview includes the events of 1584 (Aigle, epicentral intensity VIII), 1755 (Brig, epicentral intensity VIII), 1855 (Visp, epicentral intensity VIII), and 1946 (Sierre, epicentral intensity VIII for the main shock and intensity VII for the largest aftershock). The paper focuses mainly on primary and secondary effects in the epicentral region, providing the key data and a general characterization of the event. Generally, primary effects such as the reaction of the population and impact on buildings took more focus in the past. Thus building damage is more frequently described in historic documents. However, we also found a number of sources describing secondary effects such as landslides, snow avalanches, and liquefaction. Since the sources may be useful, we include citations of these documents. The 1584 Aigle event, for example, produced exceptional movements in Lake Geneva, which can be explained by an expanded sub aquatic slide with resultant tsunami and seiche. The strongest of the aftershocks of the 1584 event triggered a destructive landslide covering the villages Corbeyrier and Yvorne, VD. All macroseismic data on the discussed events are accessible through the webpage of the Swiss Seismological Service ( http://www.seismo.ethz.ch )