Hydro-sedimentary parameters measurements within the proglacial area of the Bossons glacier (Mont-Blanc massif, France)

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Bibliographic Details
Main Authors: Guillon, Hervé, Godon, Cécile, Buoncristiani, Jean-François, Mugnier, Jean-Louis
Format: Dataset Open Access
Language:en
Published: PANGAEA 2015
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author Guillon, Hervé
Godon, Cécile
Buoncristiani, Jean-François
Mugnier, Jean-Louis
author_facet Guillon, Hervé
Godon, Cécile
Buoncristiani, Jean-François
Mugnier, Jean-Louis
collection Datos científicos de ciencias marinas y ambientales
contents This dataset presents hydro-sedimentary data within the Bossons glacier proglacial area. Bossons glacier is rapidly retreating and its proglacial area is deglaciated for ~ 30 years. It is an intriguing location to study periglacial, proglacial and subglacial erosion processes which requires estimating Total Dissolved Solid (TDS) and Total Suspended Solid (TSS) concentrations, and discharge. Measurements were performed at three distinct locations within Bosson glacier watershed : Bossons downstream (BDS), Bossons upstream (BUS) and Crosette (CRO). The latter is located at the glacier termini whereas BDS and BUS stations are farther downstream from the glacier, at 1.5 and 1.15 km, respectively .
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_848151
institution PANGAEA
language en
publishDate 2015
publisher PANGAEA
record_format pangaea
spellingShingle Hydro-sedimentary parameters measurements within the proglacial area of the Bossons glacier (Mont-Blanc massif, France)
Guillon, Hervé
Godon, Cécile
Buoncristiani, Jean-François
Mugnier, Jean-Louis

This dataset presents hydro-sedimentary data within the Bossons glacier proglacial area. Bossons glacier is rapidly retreating and its proglacial area is deglaciated for ~ 30 years. It is an intriguing location to study periglacial, proglacial and subglacial erosion processes which requires estimating Total Dissolved Solid (TDS) and Total Suspended Solid (TSS) concentrations, and discharge. Measurements were performed at three distinct locations within Bosson glacier watershed : Bossons downstream (BDS), Bossons upstream (BUS) and Crosette (CRO). The latter is located at the glacier termini whereas BDS and BUS stations are farther downstream from the glacier, at 1.5 and 1.15 km, respectively .
title Hydro-sedimentary parameters measurements within the proglacial area of the Bossons glacier (Mont-Blanc massif, France)
topic
url https://doi.org/10.1594/PANGAEA.848151