Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén

The geomorphologic analysis of the study area led to distinguish some formations not considered in previous geological research, as well as to explain the characteristics of the present relief. Thirteen principal geomorphic units produced by different geomorphic processes are recognized. Their varie...

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Autores principales: González Díaz, E.F., Folguera, A.
Formato: Artículo publishedVersion
Publicado: 2011
Materias:
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
http://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v68_n1_p17_GonzalezDiaz_oai
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spelling I28-R145-paper_00044822_v68_n1_p17_GonzalezDiaz_oai2020-10-19 González Díaz, E.F. Folguera, A. 2011 The geomorphologic analysis of the study area led to distinguish some formations not considered in previous geological research, as well as to explain the characteristics of the present relief. Thirteen principal geomorphic units produced by different geomorphic processes are recognized. Their variety and incidence through the time are expressed in the glacial morphogenesis concentrated in the western part of the Cordillera del Viento, in the volcanic landscape that predominates in the northern and eastern sectors (calderas, volcanoes, lava flows), in the structural control that defines the morphology of the fluvial process in the central zone and a firstly recognized important landslide to the north of Tricao Malal. As a result of the methodology employed two geological units of different age in the western part of the Tromen-Waile volcanic field were distinguished, which were initially interpreted as a single formation. A limited but consistent structural analysis of the region is also included. Fil:Folguera, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. application/pdf http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Rev. Asoc. Geol. Argent. 2011;68(1):17-32 drainage basin fluvial process geomorphology landslide morphogenesis structural analysis Argentina Cordillera del Viento Neuquen Tromen Volcano Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion http://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v68_n1_p17_GonzalezDiaz_oai
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-145
collection Repositorio Digital de la Universidad de Buenos Aires (UBA)
topic drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
spellingShingle drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
González Díaz, E.F.
Folguera, A.
Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
topic_facet drainage basin
fluvial process
geomorphology
landslide
morphogenesis
structural analysis
Argentina
Cordillera del Viento
Neuquen
Tromen Volcano
description The geomorphologic analysis of the study area led to distinguish some formations not considered in previous geological research, as well as to explain the characteristics of the present relief. Thirteen principal geomorphic units produced by different geomorphic processes are recognized. Their variety and incidence through the time are expressed in the glacial morphogenesis concentrated in the western part of the Cordillera del Viento, in the volcanic landscape that predominates in the northern and eastern sectors (calderas, volcanoes, lava flows), in the structural control that defines the morphology of the fluvial process in the central zone and a firstly recognized important landslide to the north of Tricao Malal. As a result of the methodology employed two geological units of different age in the western part of the Tromen-Waile volcanic field were distinguished, which were initially interpreted as a single formation. A limited but consistent structural analysis of the region is also included.
format Artículo
Artículo
publishedVersion
author González Díaz, E.F.
Folguera, A.
author_facet González Díaz, E.F.
Folguera, A.
author_sort González Díaz, E.F.
title Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_short Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_full Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_fullStr Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_full_unstemmed Geomorphologic analysis of the lower and middle section of the drainage basin of the Curri Leuvúriver, Neuquén
title_sort geomorphologic analysis of the lower and middle section of the drainage basin of the curri leuvúriver, neuquén
publishDate 2011
url http://hdl.handle.net/20.500.12110/paper_00044822_v68_n1_p17_GonzalezDiaz
http://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v68_n1_p17_GonzalezDiaz_oai
work_keys_str_mv AT gonzalezdiazef geomorphologicanalysisofthelowerandmiddlesectionofthedrainagebasinofthecurrileuvuriverneuquen
AT folgueraa geomorphologicanalysisofthelowerandmiddlesectionofthedrainagebasinofthecurrileuvuriverneuquen
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