Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W)
Considering the high concentration of rock avalanches in the northern part of the Neuquén province of Argentina (36°-38°S and 70°-71°W) and their association with lacustrine basins forming natural dams, their catastrophic collapse seems not to be such a common process as could be expected for these...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v62_n3_p460_Penna http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p460_Penna |
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paper:paper_00044822_v62_n3_p460_Penna2023-06-08T14:26:04Z Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) Penna, Ivanna Marina Folguera, Andrés Neuquén Outburst flood Rock avalanches Sedimentary analysis alluvial deposit collapse structure flooding fluvial geomorphology outburst Postglacial river terrace rock avalanche sedimentology Argentina Neuquen South America Considering the high concentration of rock avalanches in the northern part of the Neuquén province of Argentina (36°-38°S and 70°-71°W) and their association with lacustrine basins forming natural dams, their catastrophic collapse seems not to be such a common process as could be expected for these cases. The present work depicts the area immediately affected by the outburst flood corresponding to the Navarrete dam catastrophic collapse (175 × 106 m3), through a sedimentological analysis, generated since the arroyo Colorado was blocked due to a rock avalanche deposit during not well constrained postglacial times. The outburst flood dispersion is initially inferred based on morphological criteria and then determined from a sedimentological analysis of its matrix. Furthermore, the matrix is compared to that of the fluvial terraces, which have been sampled along the arroyo Colorado. This comparison shows that even though differences among them are not so significant through most of the study area, matrix frequency starts to be distinctive from the most distant point of sampling. Fil:Penna, I.M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Folguera, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2007 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v62_n3_p460_Penna http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p460_Penna |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Neuquén Outburst flood Rock avalanches Sedimentary analysis alluvial deposit collapse structure flooding fluvial geomorphology outburst Postglacial river terrace rock avalanche sedimentology Argentina Neuquen South America |
spellingShingle |
Neuquén Outburst flood Rock avalanches Sedimentary analysis alluvial deposit collapse structure flooding fluvial geomorphology outburst Postglacial river terrace rock avalanche sedimentology Argentina Neuquen South America Penna, Ivanna Marina Folguera, Andrés Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) |
topic_facet |
Neuquén Outburst flood Rock avalanches Sedimentary analysis alluvial deposit collapse structure flooding fluvial geomorphology outburst Postglacial river terrace rock avalanche sedimentology Argentina Neuquen South America |
description |
Considering the high concentration of rock avalanches in the northern part of the Neuquén province of Argentina (36°-38°S and 70°-71°W) and their association with lacustrine basins forming natural dams, their catastrophic collapse seems not to be such a common process as could be expected for these cases. The present work depicts the area immediately affected by the outburst flood corresponding to the Navarrete dam catastrophic collapse (175 × 106 m3), through a sedimentological analysis, generated since the arroyo Colorado was blocked due to a rock avalanche deposit during not well constrained postglacial times. The outburst flood dispersion is initially inferred based on morphological criteria and then determined from a sedimentological analysis of its matrix. Furthermore, the matrix is compared to that of the fluvial terraces, which have been sampled along the arroyo Colorado. This comparison shows that even though differences among them are not so significant through most of the study area, matrix frequency starts to be distinctive from the most distant point of sampling. |
author |
Penna, Ivanna Marina Folguera, Andrés |
author_facet |
Penna, Ivanna Marina Folguera, Andrés |
author_sort |
Penna, Ivanna Marina |
title |
Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) |
title_short |
Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) |
title_full |
Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) |
title_fullStr |
Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) |
title_full_unstemmed |
Identification of the area immediately affected by outburst flood of the Laguna Navarrete, Province of Neuquén (36°30′S-71°W) |
title_sort |
identification of the area immediately affected by outburst flood of the laguna navarrete, province of neuquén (36°30′s-71°w) |
publishDate |
2007 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v62_n3_p460_Penna http://hdl.handle.net/20.500.12110/paper_00044822_v62_n3_p460_Penna |
work_keys_str_mv |
AT pennaivannamarina identificationoftheareaimmediatelyaffectedbyoutburstfloodofthelagunanavarreteprovinceofneuquen3630s71w AT folgueraandres identificationoftheareaimmediatelyaffectedbyoutburstfloodofthelagunanavarreteprovinceofneuquen3630s71w |
_version_ |
1768545168610295808 |