Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud

Analysing of longitudinal profiles of coastal river channels in South Brittany allows to highlight relationships between fluvial dynamics, lithology and tectonics. Profile shapes and knickzones (high gradient sections) show that headward incision is due to tectonics, but controlled by lithology. In...

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Main Author: Jean-Pierre Larue
Format: Article
Language:English
Published: Physio-Géo 2014-01-01
Series:Physio-Géo
Subjects:
Online Access:https://journals.openedition.org/physio-geo/3798
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author Jean-Pierre Larue
author_facet Jean-Pierre Larue
author_sort Jean-Pierre Larue
collection DOAJ
description Analysing of longitudinal profiles of coastal river channels in South Brittany allows to highlight relationships between fluvial dynamics, lithology and tectonics. Profile shapes and knickzones (high gradient sections) show that headward incision is due to tectonics, but controlled by lithology. In little hard rocks, like Brioverian micaschists, profiles are concave- upwards and without any knickzone. While in hard rocks, such as granites or gneiss, large knickzones disrupt the longitudinal profiles. Along the north-south rivers which crosses various lithology,the upstream reaches present longitudinal profiles with high concavity and shallow incision, whereas the downstream reaches are marked by week concavity, important knickzones and deeper incision. This contrast indicates a steady state evolution in the upstream reach and a desequilibrium in the downstream reach.
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spelling doaj-art-c2de658ee89543eabaa5d85e4d0c90202024-12-09T13:28:56ZengPhysio-GéoPhysio-Géo1958-573X2014-01-018496510.4000/physio-geo.3798Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sudJean-Pierre LarueAnalysing of longitudinal profiles of coastal river channels in South Brittany allows to highlight relationships between fluvial dynamics, lithology and tectonics. Profile shapes and knickzones (high gradient sections) show that headward incision is due to tectonics, but controlled by lithology. In little hard rocks, like Brioverian micaschists, profiles are concave- upwards and without any knickzone. While in hard rocks, such as granites or gneiss, large knickzones disrupt the longitudinal profiles. Along the north-south rivers which crosses various lithology,the upstream reaches present longitudinal profiles with high concavity and shallow incision, whereas the downstream reaches are marked by week concavity, important knickzones and deeper incision. This contrast indicates a steady state evolution in the upstream reach and a desequilibrium in the downstream reach.https://journals.openedition.org/physio-geo/3798lithologylongitudinal profilesknickzonesheadward incisiontectonicsBretagne
spellingShingle Jean-Pierre Larue
Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud
Physio-Géo
lithology
longitudinal profiles
knickzones
headward incision
tectonics
Bretagne
title Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud
title_full Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud
title_fullStr Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud
title_full_unstemmed Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud
title_short Profils longitudinaux et ruptures de pente : enseignements géomorphologiques en Bretagne du sud
title_sort profils longitudinaux et ruptures de pente enseignements geomorphologiques en bretagne du sud
topic lithology
longitudinal profiles
knickzones
headward incision
tectonics
Bretagne
url https://journals.openedition.org/physio-geo/3798
work_keys_str_mv AT jeanpierrelarue profilslongitudinauxetrupturesdepenteenseignementsgeomorphologiquesenbretagnedusud