A review of historical lahars, floods, and landslides in the Prêcheur river catchment (Montagne Pelée volcano, Martinique island, Lesser Antilles)

Author:

Aubaud Cyril1,Athanase Jean-Elie1,Clouard Valérie1,Barras Anne-Valérie23,Sedan Olivier4

Affiliation:

1. Observatoire Volcanologique et Sismologique de Martinique, Institut de Physique du Globe de Paris, PRES Sorbonne Paris Cité, UMR CNRS 7154, Morne des Cadets, Fonds St Denis, 97250, Saint Pierre, Martinique, French West Indies.

2. BRGM Martinique, 4 Lot. Miramar, Route Pointe des Nègres, 97200 Fort de France, Martinique, F.W.I.

3. BRGM Service géologique régional Alsace, 15 rue du Tanin, Parc-Club des Tanneries, Lingolsheim, BP 177, 67834 Tanneries cedex, France

4. BRGM Orléans, 3 rue Claude Guillemin, BP36009, 45060 Orléans cedex 2, France

Abstract

Abstract The Prêcheur river catchment belongs to the Montagne Pelée volcano massif located in the north of Martinique island, in the Lesser Antilles arc. In June 19–20, 2010 two high-discharge lahars overflowed and partially damaged the Prêcheur bridge, interrupting the road traffic for several days, and inundating part of the Abymes quarter. These non-eruptive, rain-triggered lahars were the consequence of the mobilization of loose volcanic material accumulated in the river bed by a massive landslide of the Samperre cliff that occurred on May 11, 2010. In order to improve lahar risk assessment for the Prêcheur river, we review the existing knowledge on lahars and floods for the period 1851–2011. We improved the database mainly on the basis of geophysical (seismic and acoustic) data for the most recent period (1980-present). We show that: (1) the largest event ever observed in Prêcheur is the eruption-related lahar of May 8, 1902 at 06:00 UTC, (2) high-discharge, non-eruptive lahars able to partially destroy or submerge the bridge occur every 10.3 years in average since 1950, (3) geophysical records show that there are more low magnitude lahars than previously recognized because witness accounts report the larger events and therefore filter out the smaller ones; by contrast geophysical instruments are able to detect both high and low magnitude events, (4) the recent paroxysms of 2009–2010 belong to a landslide-lahar crisis which started in 2004; the onset of the landslide-lahar crisis was unnoticed by the population due to the low magnitude of the events. The results of this compilation stress the importance of the presence of geophysical instrumentation sufficiently close to the river for monitoring small scale landslides and lahars. Indeed, these low magnitude events are likely to be unnoticed by the local population and therefore likely to be absent from the collective memory and local newspapers. However, they can inform about the imminence of more significant events, as observed in 1980 and 2010.

Publisher

EDP Sciences

Subject

Geology

Reference44 articles.

1. Rapport sur le glissement du Piton Marcel du 11 mai 2010;Aubaud,2010

2. Rapport sur la coulée de boue de la rivière du Prêcheur du 17 mai 2010;Aubaud,2010

3. Atlan Y. Besson J.-C. Humbert M. (1983). – Evolution des reliefs en liaison avec la sécurité et l’aménagement du territoire en Martinique. – Rapport BRGM 83-ANT-016, 58 p. Available at: http://www.brgm.fr/publication/pubDetailRapportSP.jsp?id=RSP-BRGM/83-ANT-016.

4. Barras A.-V. (2010). – Rapport circonstancié sur les coulées de boue torrentielles des 19 et 20 juin 2010 au Prêcheur dans le cadre de la procédure de reconnaissance de l’état de catastrophe naturelle. Rapport final. – Rapport BRGM/RP-58826-FR, 36p. Available at: http://www.brgm.fr/publication/pubDetailRapportSP.jsp?id=RSP-BRGM/RP-58826-FR.

5. Rapport sur la reconnaissance en hélicoptère effectuée au-dessus de la rivière du Prêcheur le 25 juin 2010;Barras,2010

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