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                <title xml:lang="en">A record of the fluctuations of the "mer de glace" during the Holocene: the "Côte du Piget" in the Chamonix valley</title>
                <title xml:lang="fr">Un témoin des fluctuations de la Mer de Glace durant l’Holocène : la Côte du Piget en vallée de Chamonix</title>
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                    <forename type="first">Jean-François</forename>
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                <term xml:lang="en">Little Ice Age</term>
                <term xml:lang="en">geoelectric tomography</term>
                <term xml:lang="en">geomorphology</term>
                <term xml:lang="en">hamlet destruction</term>
                <term xml:lang="fr">Petit Âge Glaciaire</term>
                <term xml:lang="fr">Mer de Glace</term>
                <term xml:lang="fr">tomographie géoélectrique</term>
                <term xml:lang="fr">géomorphologie</term>
                <term xml:lang="fr">destruction d’habitats</term>
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              <p>The "Côte du Piget", near the village of Les Bois in the Chamonix valley, is covered by a thick moraine from the right bank of the Mer de Glace. This moraine, essentially comprised of granitic debris, was progressively deposited on a limestone ridge after the Younger Dryas glacial episode about 12,000 years ago. A geoelectrical survey conducted in 2018 and 2019 enabled the detection of the underlying limestone bedrock, the surface of which is characterised by a very low electrical resistivity. It also allowed to identify the base of moraines with a granitic component from the Little Ice Age (LIA) thanks to their very high electrical resistivity. Most of these moraines were deposited during the paroxysmal phases of the LIA in the xviith and xixth centuries. Tomographic models giving the variation of intrinsic resistivity up to a depth of about 40 m are built by inverse method using surface measurements of apparent resistivity. The structural interpretation we propose is compared to the known glacial episodes of the Holocene and leads us to present a model of moraine filling from the Younger Dryas to the end of the LIA. The location of two settlements destroyed by the glacial advance in the xviith century is clarified in the light of this structural interpretation.</p>
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              <p>Résumé : La « Côte du Piget », près du village des Bois dans la vallée de Chamonix, est recouverte par une épaisse moraine provenant de la rive droite de la Mer de Glace. Cette moraine essentiellement constituée de débris granitiques s’est progressivement déposée sur un promontoire calcaire après l’épisode glaciaire du Dryas récent il y a environ 12000 ans. Une prospection géo‑électrique conduite en 2018 et 2019 a permis de détecter le socle calcaire sous‑jacent dont la surface est caractérisée par une très faible résistivité électrique. Elle a également permis de repérer la base des moraines à composante granitique du Petit Age Glaciaire (PAG) en raison de leur très forte résistivité électrique. Ces moraines se sont déposées principalement durant la phase paroxysmale PAG aux xviie et xixe siècles. Des modèles tomographiques donnant la variation de la résistivité intrinsèque jusqu’à une profondeur d’environ 40 m sont obtenus par méthode inverse à partir des mesures de résistivité apparente faites en surface. L’interprétation structurale que nous proposons est confrontée aux épisodes glaciaires connus de l’Holocène et nous conduit à présenter un modèle de remplissage morainique depuis le Dryas récent jusqu’à la fin du PAG. La localisation des deux villages qui ont disparu à cet endroit devant l’avancée glaciaire du xviie siècle est précisée à la lumière de cette interprétation structurale.</p>
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