A quantification of the glacial imprint on relief development in the French western Alps

Accurate determination of the Cp values in polymers or other poor heat conduc- tors require relatively long period durations in the order of 3 to 6 rain, even if small

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Permafrost extension modeling in rock slope since the Last Glacial Maximum: application to the large Séchilienne landslide (French Alps).... Permafrost extension modeling in a rock

Concentrations of Water Soluble Organic Carbon (WSOC) and WSOC fraction to Organic Carbon (OC) were measured at two urban sites in valleys of the French Alps dur- ing a period of

Table DR1, Age of the Tertiary lithostratigraphic units inferred from magnetostratigraphic studies and others methods, Table DR 2, The migration of the pinch-out of the

5: Modelled rebound of the W-Alps in response to Quaternary erosion (calculated for T e = 10 km and mass removal equivalent to basin fill over the last 1.8 Ma). Rebound is shown

This paper aims at identifying trends in the vulnerability of Alpine forest ecosystems to fire at different scales (tree species, stand level and biogeographic level) and according

In  der  lebensstilforschung  und  verschiedenen  disziplinen  der  Raumforschung