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Lambesc earthquake 1909

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Journal Article

Commentaire à la note de D. Chardon et O. Bellier intitulée « Geological boundary conditions of the 1909 Lambesc (Provence, France) earthquake : structure and evolution of the Trévaresse ridge anticline »: « Cadre géologique du séisme de Lambesc du 11 juin 1909 (Provence, France ; structure et évolution de l’anticlinal de la Trévaresse »

Maurice Mattauer
Published: 01 January 2005
Bulletin de la Société Géologique de France (2005) 176 (1): 121–122.
DOI: https://doi.org/10.2113/176.1.121
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Geological boundary conditions of the 1909 Lambesc (Provence, France) earthquake : structure and evolution of the Trévaresse ridge anticline

Dominique Chardon, Olivier Bellier
Published: 01 September 2003
Bulletin de la Société Géologique de France (2003) 174 (5): 497–510.
DOI: https://doi.org/10.2113/174.5.497
...Dominique Chardon; Olivier Bellier Abstract The 06/11/1909, Lambesc, M=6 earthquake is the strongest instrumental seismic event recorded in French history. A review of the geology of the epicentral area combined with detailed field mapping and structural analysis allows constraining the tectonic...
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The analysis of historical seismograms: an important tool for seismic hazard assessment. Case histories from French and Italian earthquakes

Nicola Alessandro Pino
Published: 01 July 2011
Bulletin de la Société Géologique de France (2011) 182 (4): 367–379.
DOI: https://doi.org/10.2113/gssgfbull.182.4.367
... analysis of selected significant historical earthquakes occurred during the first decades of the XX th century, including ( A) the December 28, 1908, Messina straits (southern Italy), ( B) the June 11, 1909, Lambesc (southern France) – both of which are the strongest ever recorded instrumentally...
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First paleoseismological constraints on the strongest earthquake in France (Provence) in the twentieth century

Dominique Chardon, Daniel Hermitte, Frédéric Nguyen, Olivier Bellier
Journal: Geology
Published: 01 November 2005
Geology (2005) 33 (11): 901–904.
DOI: https://doi.org/10.1130/G21713.1
...Dominique Chardon; Daniel Hermitte; Frédéric Nguyen; Olivier Bellier Abstract We have identified surface ruptures of M ≥ 6 earthquakes on a branch of the propagating reverse fault system that produced the strongest event recorded in France during the twentieth century (1909 Lambesc earthquake...
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Isovalues of macroseismic intensities produced by the historic <span class="search-highlight">1909</span> <span class="search-highlight">Lambesc</span>...

Isovalues of macroseismic intensities produced by the historic 1909 Lambesc...

Published: 01 March 2014
Figure 6. Isovalues of macroseismic intensities produced by the historic 1909 Lambesc earthquake. (Source: SisFrance .)
Journal Article

Morphostructural evolution of the Luberon since the Miocene (SE France)

Georges Clauzon, Thomas-Jules Fleury, Olivier Bellier, Stéphane Molliex, Ludovic Mocochain, Jean-Pierre Aguilar
Published: 01 March 2011
Bulletin de la Société Géologique de France (2011) 182 (2): 95–110.
DOI: https://doi.org/10.2113/gssgfbull.182.2.95
... the Alpine phase did not modify the morphology, deformation migrated southwards from the Luberon. Some of the faults are still active, as shown by the 1909 Lambesc earthquake (11 June 1909; 6 Mw), which triggered the reactivation of the Trévaresse fault. * Corresponding author: [email protected]...
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Comparison of observed intensities and predicted isoseismals for the 11 Jun...

Comparison of observed intensities and predicted isoseismals for the 11 Jun...

Published: 01 December 2004
Figure 9. Comparison of observed intensities and predicted isoseismals for the 11 June 1909 Lambesc (Provence) earthquake. Points are observed intensities from the SIRENE database and lines are predicted isoseismals that take geological conditions into account.
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Example of theoretical frequency response for different components and stat...

Example of theoretical frequency response for different components and stat...

Published: 01 July 2011
F ig . 2. – Example of theoretical frequency response for different components and stations. These curves are relative to instruments that recorded the July 11, 1909, Lambesc earthquake and represent the theoretical response for different instruments including Wiechert, Bosch, and Vicentini
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Evaluation of the level of damage for the <span class="search-highlight">Lambesc</span> <span class="search-highlight">earthquake</span> scenario consi...

Evaluation of the level of damage for the Lambesc earthquake scenario consi...

Published: 01 March 2014
Figure 8. Evaluation of the level of damage for the Lambesc earthquake scenario considering (a) 1909 urbanization and (b) 2008 urbanization. Damage is grouped by D 0 + D 1 (left). D 2 + D 3 (middle), and D 4 + D 5 (right column) EMS‐98 damage scale. The color scale gives the number
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Summary of the results obtained by Baroux et al. [2003] for the <span class="search-highlight">Lambesc</span>...

Summary of the results obtained by Baroux et al. [2003] for the Lambesc...

Published: 01 July 2011
F ig . 8. – Summary of the results obtained by Baroux et al. [2003] for the Lambesc 1909 earthquake. The combination with historical and geodetic data suggests that this event was generated by the western segment of the Trévaresse fold. The preferred source is a 106 km 2 fault, extending
Journal Article

Introduction to “PROVENCE 2009” Seismic risk in regions of moderate seismicity: from hazard to vulnerability

Olivier Bellier
Published: 01 July 2011
Bulletin de la Société Géologique de France (2011) 182 (4): 277–278.
DOI: https://doi.org/10.2113/gssgfbull.182.4.277
...., Bellier [2009]; http://provence2009.eccorev.fr ; www.seisme-1909-provence.fr ). On June 11 th , 1909, the M=6 Lambesc earthquake occurred in Provence (SE France). It is one of the highest intensity earthquakes that shocked the metropolitan territory of France within the historical scale [e.g...
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Macroscale Vulnerability Assessment of Cities Using Association Rule Learning

I. Riedel, P. Guéguen, F. Dunand, S. Cottaz
Published: 01 March 2014
Seismological Research Letters (2014) 85 (2): 295–305.
DOI: https://doi.org/10.1785/0220130148
...Figure 6. Isovalues of macroseismic intensities produced by the historic 1909 Lambesc earthquake. (Source: SisFrance .) ...
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The five most significant <span class="search-highlight">earthquakes</span> from 2010 to 2019. (a) Map at nationa...

The five most significant earthquakes from 2010 to 2019. (a) Map at nationa...

Published: 23 April 2021
is the 1909 Lambesc earthquake. FMD is the Moyenne Durance Fault zone. (f) The ML 5.1 Barcelonnette earthquake on April 7, 2014. The red dashed line symbolizes the French-Italian border.
Journal Article

The 23 April 23 1909 Benavente (Portugal) M 6.3 Earthquake

J. F. B. D. Fonseca, S. P. Vilanova
Published: 01 May 2010
Seismological Research Letters (2010) 81 (3): 534–536.
DOI: https://doi.org/10.1785/gssrl.81.3.534
... limit of the LTV region. In 1909, the Benavente earthquake ( Figure 1 ) clearly established the LTV region as a seismic source zone ( Choffat and Bensaude 1912 ). On 23 April 1909 at 5:03 p.m., the towns of Benavente, Samora Correia, and Santo Estevao ( Figure 2 ), on the south margin...
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Foreword

Maurice Haessler
Published: 01 November 2010
Bulletin de la Société Géologique de France (2010) 181 (6): 475.
DOI: https://doi.org/10.2113/gssgfbull.181.6.475
.... The historical earthquakes, such as the Lambesc earthquake in 1909, remind us of the reality of this risk. Located about forty kilometers north of Aix-en-Provence, the Cadarache Center gathers a number of research facilities, associated to nuclear service facilities (in operation or under construction). Most...
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Geodynamics of the France Southeast Basin

Xavier Le Pichon, Claude Rangin, Youri Hamon, Nicolas Loget, Jin Ying Lin, Louis Andreani, Nicolas Flotte
Published: 01 November 2010
Bulletin de la Société Géologique de France (2010) 181 (6): 477–501.
DOI: https://doi.org/10.2113/gssgfbull.181.6.477
... instrumentally measured earthquake (M w 5.7 to 6.1, preferred value of 6 and M s 6.0) is the 1909 Lambesc earthquake (fig. 1 ). It produced intensity IX effects 30 km north of Marseille [ Baroux et al ., 2003 ]. This is a reverse earthquake related to the Trévaresse range with a 6 km hypocenter...
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A Probabilistic Approach to Seismic Hazard in Metropolitan France

Sylvie Marin, Jean-Philippe Avouac, Marc Nicolas, Antoine Schlupp
Published: 01 December 2004
Bulletin of the Seismological Society of America (2004) 94 (6): 2137–2163.
DOI: https://doi.org/10.1785/0120030232
...Figure 9. Comparison of observed intensities and predicted isoseismals for the 11 June 1909 Lambesc (Provence) earthquake. Points are observed intensities from the SIRENE database and lines are predicted isoseismals that take geological conditions into account. ...
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Station COI: Dusting Off an Old Seismic Station

Susana Custódio, Josep Batlló, Décio Martins, Fábio Antunes, João Narciso, Sara Carvalho, Vânia Lima, Fernando C. Lopes, Paulo Ribeiro, Reinoud Sleeman, E. Ivo Alves, Celeste R. Gomes
Published: 01 September 2012
Seismological Research Letters (2012) 83 (5): 863–869.
DOI: https://doi.org/10.1785/0220120014
.... Teves‐Costa P. Morales J. ( 2005 ). Moment tensor in version with single‐component historical seismograms: The 1909 Benavente (Portugal) and Lambesc (France) earthquakes , Geophys. J. Int. 162 , 850 – 858 , doi: 10.1111/j.1365‐246X.2005.02680.x . Teves‐Costa P. Batlló J...
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The Source of the 30 October 1930 M w 5.8 Senigallia (Central Italy) Earthquake: A Convergent Solution from Instrumental, Macroseismic, and Geological Data

Paola Vannoli, Gianfranco Vannucci, Fabrizio Bernardi, Barbara Palombo, Graziano Ferrari
Published: 19 May 2015
Bulletin of the Seismological Society of America (2015) 105 (3): 1548–1561.
DOI: https://doi.org/10.1785/0120140263
..., and focal mechanism, by carefully retrieving, processing, and analyzing all available seismograms (e.g., Baroux et al. , 2003 , for the 1909 Lambesc earthquake, southern France; Stich et al. , 2005 , for the 1909 Benavente earthquake, central Portugal; Pino et al. , 2008 , for the 1930 Irpinia...
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Large Holocene Earthquakes in the Lower Tagus Valley Fault Zone, Central Portugal

G. M. Besana-Ostman, S. P. Vilanova, E. S. Nemser, A. Falcao-Flor, S. Heleno, H. Ferreira, J. D. Fonseca
Published: 01 January 2012
Seismological Research Letters (2012) 83 (1): 67–76.
DOI: https://doi.org/10.1785/gssrl.83.1.67
...-size earthquake affected several towns within the Lower Tagus Valley with major destruction in the town of Benavente and two other villages ( Fonseca and Vilanova 2010 ). The earthquake, known as the 1909 Benavente earthquake, was studied rigorously by both contemporaneous ( Chofat and Bensaude 1912...
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