The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina

At the southern end of the Sierra de la Puntilla Range in northern Neuquén province, extensive deposits of "tilloid" features in a morphological environment with hummocky-topography were observed. Previous studies suggest their relation with glacial morphogenesis (moraines; tills). We prop...

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Detalles Bibliográficos
Publicado: 2003
Materias:
Ailinco
C° Papas
De la Puntilla Range
Northern Neuquén
Rock-avalanches
Seismic shock
geomorphology
gravity
landslide
rock avalanche
seismic hazard
trigger mechanism
Argentina
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v58_n2_p194_ConzalezDiaz
http://hdl.handle.net/20.500.12110/paper_00044822_v58_n2_p194_ConzalezDiaz
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id paper:paper_00044822_v58_n2_p194_ConzalezDiaz
record_format dspace
spelling paper:paper_00044822_v58_n2_p194_ConzalezDiaz2023-06-08T14:25:39Z The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina Ailinco C° Papas De la Puntilla Range Northern Neuquén Rock-avalanches Seismic shock geomorphology gravity landslide rock avalanche seismic hazard trigger mechanism Argentina At the southern end of the Sierra de la Puntilla Range in northern Neuquén province, extensive deposits of "tilloid" features in a morphological environment with hummocky-topography were observed. Previous studies suggest their relation with glacial morphogenesis (moraines; tills). We propose instead here their relationship to large gravitational movements triggered by seismic shock, and we distinguish two rock-avalanches and a third considered as a minor landslide. The most important is the "Cerro Papas rock-avalanche" which occurred on its western slope. The "Ailinco rock-avalanche" is situated on the southern end of the Puntilla Range, and the "Las Olletas landslide" is located in the proximity of Aguas Calientes. The landslides are described merely in terms of their principal morphological features. Other secondary landforms (of regional landscape) described are related to glaciation, permafrost environment and minor mass-wasting processes. 2003 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v58_n2_p194_ConzalezDiaz http://hdl.handle.net/20.500.12110/paper_00044822_v58_n2_p194_ConzalezDiaz
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Ailinco
C° Papas
De la Puntilla Range
Northern Neuquén
Rock-avalanches
Seismic shock
geomorphology
gravity
landslide
rock avalanche
seismic hazard
trigger mechanism
Argentina
spellingShingle Ailinco
C° Papas
De la Puntilla Range
Northern Neuquén
Rock-avalanches
Seismic shock
geomorphology
gravity
landslide
rock avalanche
seismic hazard
trigger mechanism
Argentina
The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina
topic_facet Ailinco
C° Papas
De la Puntilla Range
Northern Neuquén
Rock-avalanches
Seismic shock
geomorphology
gravity
landslide
rock avalanche
seismic hazard
trigger mechanism
Argentina
description At the southern end of the Sierra de la Puntilla Range in northern Neuquén province, extensive deposits of "tilloid" features in a morphological environment with hummocky-topography were observed. Previous studies suggest their relation with glacial morphogenesis (moraines; tills). We propose instead here their relationship to large gravitational movements triggered by seismic shock, and we distinguish two rock-avalanches and a third considered as a minor landslide. The most important is the "Cerro Papas rock-avalanche" which occurred on its western slope. The "Ailinco rock-avalanche" is situated on the southern end of the Puntilla Range, and the "Las Olletas landslide" is located in the proximity of Aguas Calientes. The landslides are described merely in terms of their principal morphological features. Other secondary landforms (of regional landscape) described are related to glaciation, permafrost environment and minor mass-wasting processes.
title The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina
title_short The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina
title_full The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina
title_fullStr The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina
title_full_unstemmed The complex landslide of Ailinco-C° Papas-Las Olletas, northern Neuquén, Argentina
title_sort complex landslide of ailinco-c° papas-las olletas, northern neuquén, argentina
publishDate 2003
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v58_n2_p194_ConzalezDiaz
http://hdl.handle.net/20.500.12110/paper_00044822_v58_n2_p194_ConzalezDiaz
_version_ 1768543923690536960

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