Erosion in the Chilean Andes between 27°S and 39°S: Tectonic, climatic and geomorphic control

S. Carretier, V. Tolorza, M. P. Rodríguez, E. Pepin, G. Aguilar, V. Regard, J. Martinod, R. Riquelme, S. Bonnet, S. Brichau, G. Hérail, L. Pinto, M. Farías, R. Charrier, J. L. Guyot

Resultado de la investigación: Article

15 Citas (Scopus)

Resumen

The effect of mean precipitation rate on erosion is debated. Three hypotheses may explain why the current erosion rate and runoff may be spatially uncorrelated: (1) the topography has reached a steady state for which the erosion rate pattern is determined by the uplift rate pattern; (2) the erosion rate only depends weakly on runoff; or (3) the studied catchments are experiencing different transient adjustments to uplift or to climate variations. In the Chilean Andes, between 27°S and 39°S, the mean annual runoff rates increase southwards from 0.01 to 2.6 m a-1 but the catchment averaged rates of decadal erosion (suspended sediment) and millennial erosion (10Be in river sand) peak at c. 0.25 mm a-1 for runoff c. 0.5 m a-1 and then decrease while runoff keeps increasing. Erosion rates increase non-linearly with the slope and weakly with the square root of the runoff. However, sediments trapped in the subduction trench suggest a correlation between the current runoff pattern and erosion over millions of years. The third hypothesis above may explain these different erosion rate patterns; the patterns seem consistent with, although not limited to, a model where the relief and erosion rate have first increased and then decreased in response to a period of uplift, at rates controlled by the mean precipitation rate.

Idioma originalEnglish
Páginas (desde-hasta)401-418
Número de páginas18
PublicaciónGeological Society Special Publication
Volumen399
DOI
EstadoPublished - 1 ene 2015

Huella dactilar

Tectonics
erosion rate
Erosion
Runoff
runoff
erosion
tectonics
uplift
catchment
Catchments
climate variation
suspended sediment
trench
rate
Suspended sediments
relief
subduction
topography
Topography
sand

ASJC Scopus subject areas

  • Water Science and Technology
  • Ocean Engineering
  • Geology

Citar esto

Carretier, S., Tolorza, V., Rodríguez, M. P., Pepin, E., Aguilar, G., Regard, V., ... Guyot, J. L. (2015). Erosion in the Chilean Andes between 27°S and 39°S: Tectonic, climatic and geomorphic control. Geological Society Special Publication, 399, 401-418. https://doi.org/10.1144/SP399.16
Carretier, S. ; Tolorza, V. ; Rodríguez, M. P. ; Pepin, E. ; Aguilar, G. ; Regard, V. ; Martinod, J. ; Riquelme, R. ; Bonnet, S. ; Brichau, S. ; Hérail, G. ; Pinto, L. ; Farías, M. ; Charrier, R. ; Guyot, J. L. / Erosion in the Chilean Andes between 27°S and 39°S : Tectonic, climatic and geomorphic control. En: Geological Society Special Publication. 2015 ; Vol. 399. pp. 401-418.
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abstract = "The effect of mean precipitation rate on erosion is debated. Three hypotheses may explain why the current erosion rate and runoff may be spatially uncorrelated: (1) the topography has reached a steady state for which the erosion rate pattern is determined by the uplift rate pattern; (2) the erosion rate only depends weakly on runoff; or (3) the studied catchments are experiencing different transient adjustments to uplift or to climate variations. In the Chilean Andes, between 27°S and 39°S, the mean annual runoff rates increase southwards from 0.01 to 2.6 m a-1 but the catchment averaged rates of decadal erosion (suspended sediment) and millennial erosion (10Be in river sand) peak at c. 0.25 mm a-1 for runoff c. 0.5 m a-1 and then decrease while runoff keeps increasing. Erosion rates increase non-linearly with the slope and weakly with the square root of the runoff. However, sediments trapped in the subduction trench suggest a correlation between the current runoff pattern and erosion over millions of years. The third hypothesis above may explain these different erosion rate patterns; the patterns seem consistent with, although not limited to, a model where the relief and erosion rate have first increased and then decreased in response to a period of uplift, at rates controlled by the mean precipitation rate.",
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Carretier, S, Tolorza, V, Rodríguez, MP, Pepin, E, Aguilar, G, Regard, V, Martinod, J, Riquelme, R, Bonnet, S, Brichau, S, Hérail, G, Pinto, L, Farías, M, Charrier, R & Guyot, JL 2015, 'Erosion in the Chilean Andes between 27°S and 39°S: Tectonic, climatic and geomorphic control', Geological Society Special Publication, vol. 399, pp. 401-418. https://doi.org/10.1144/SP399.16

Erosion in the Chilean Andes between 27°S and 39°S : Tectonic, climatic and geomorphic control. / Carretier, S.; Tolorza, V.; Rodríguez, M. P.; Pepin, E.; Aguilar, G.; Regard, V.; Martinod, J.; Riquelme, R.; Bonnet, S.; Brichau, S.; Hérail, G.; Pinto, L.; Farías, M.; Charrier, R.; Guyot, J. L.

En: Geological Society Special Publication, Vol. 399, 01.01.2015, p. 401-418.

Resultado de la investigación: Article

TY - JOUR

T1 - Erosion in the Chilean Andes between 27°S and 39°S

T2 - Tectonic, climatic and geomorphic control

AU - Carretier, S.

AU - Tolorza, V.

AU - Rodríguez, M. P.

AU - Pepin, E.

AU - Aguilar, G.

AU - Regard, V.

AU - Martinod, J.

AU - Riquelme, R.

AU - Bonnet, S.

AU - Brichau, S.

AU - Hérail, G.

AU - Pinto, L.

AU - Farías, M.

AU - Charrier, R.

AU - Guyot, J. L.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - The effect of mean precipitation rate on erosion is debated. Three hypotheses may explain why the current erosion rate and runoff may be spatially uncorrelated: (1) the topography has reached a steady state for which the erosion rate pattern is determined by the uplift rate pattern; (2) the erosion rate only depends weakly on runoff; or (3) the studied catchments are experiencing different transient adjustments to uplift or to climate variations. In the Chilean Andes, between 27°S and 39°S, the mean annual runoff rates increase southwards from 0.01 to 2.6 m a-1 but the catchment averaged rates of decadal erosion (suspended sediment) and millennial erosion (10Be in river sand) peak at c. 0.25 mm a-1 for runoff c. 0.5 m a-1 and then decrease while runoff keeps increasing. Erosion rates increase non-linearly with the slope and weakly with the square root of the runoff. However, sediments trapped in the subduction trench suggest a correlation between the current runoff pattern and erosion over millions of years. The third hypothesis above may explain these different erosion rate patterns; the patterns seem consistent with, although not limited to, a model where the relief and erosion rate have first increased and then decreased in response to a period of uplift, at rates controlled by the mean precipitation rate.

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