Spatio-temporal variability and controlling factors for postglacial denudation rates in the Dora Baltea catchment (western Italian Alps)

Elena Serra (1, 2) , Pierre Valla (3, 1, 4) , Romain Delunel (5) , Natacha Gribenski (1, 2) , Marcus Christl (6) , Naki Akçar (7, 2)

1 OCCR - Oeschger Centre for Climate Change Research
2 Institute of Geological Sciences [Bern]
3 UGA - Université Grenoble Alpes
4 Institute of Geological Sciences [Berlin]
5 EVS - Environnement, Ville, Société
6 Ion Beam Physics [ETH Zürich]
7 UNIBE - Universität Bern / University of Bern

Disentangling the influence of lithology from the respective roles of climate, topography and tectonic forcing on catchment denudation is often challenging in mountainous landscapes due to the diversity of geomorphic processes in action and of spatial and temporal scales involved. The Dora Baltea catchment (western Italian Alps) is an ideal setting for such investigation, since its large drainage system, extending from the Mont Blanc Massif to the Po Plain, cuts across different major lithotectonic units of the western Alps, whereas this region has experienced relatively homogeneous climatic conditions and glacial history throughout the Quaternary. We acquired new 10Be-derived catchment-wide denudation rates from 18 river-sand samples collected both along the main Dora Baltea river and at the outlet of its main tributaries. The inferred denudation rates vary between 0.2 and 0.9 mm yr−1, consistent with previously published values across the European Alps. Spatial variability in denudation rates was statistically compared with topographic, environmental and geological metrics. 10Be-derived denudation rates do not correlate with modern precipitation and rock geodetic uplift. We find, rather, that catchment topography, in turn conditioned by bedrock structures and erodibility (lithotectonic origin) and glacial overprint, is the main driver of 10Be-derived denudation patterns. We calculated the highest denudation rate for the Mont Blanc Massif, whose granitoid rocks and long-term tectonic uplift support high elevations, steep slopes and high relief and thus favour intense glacial and periglacial processes and recurring rockfall events. Finally, our results, in agreement with modern sediment budgets, demonstrate that the high sediment input from the Mont Blanc catchment dominates the Dora Baltea sediment flux, explaining the constant low 10Be concentrations measured along the Dora Baltea course even downstream the multiple junctions with tributary catchments.

Domaines: Géomorphologie

Elena Serra, Pierre Valla, Romain Delunel, Natacha Gribenski, Marcus Christl, et al.. Spatio-temporal variability and controlling factors for postglacial denudation rates in the Dora Baltea catchment (western Italian Alps). Earth Surface Dynamics, 2022, 10 (3), pp.493-512. ⟨10.5194/esurf-10-493-2022⟩. ⟨hal-03703484⟩