Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina

Autores
Abascal, Liliana del Valle; Gonzalez Bonorino, Gustavo
Año de publicación
2006
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The eastern foothills of the Central Andes, known as the Subandean Ranges, in Peru, Bolivia, and northwestern Argentina, are characterized by heavy rainfall, weakly cemented substrate rocks, thick regoliths, and bedding planes parallel to mountain slopes, features that create serious landslide hazards (Multinational Andean Project: Geoscience for Andean Communities, http://www.pma-map.com). A moderately sized landslide (the Termas Hill landslide) occurred in August 2003 on a slope of the Andean foothills in northwestern Argentina (Figure 1). The slide disrupted regolith and rock, leaving a steepwalled scarp and severing a 130-m-long segment of forest road. The sliding block travelled downslope a few tens of meters, undergoing fragmentation and torsion. On the basis of a topographic survey and structural evidence, this article discusses the geometry and kinematics of the Termas Hill landslide.
Fil: Abascal, Liliana del Valle. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Gonzalez Bonorino, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Materia
ANDES
ARGENTINA
LANDSLIDE
LANDSLIDE HAZARD
RISK
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/162086
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Kinematics of a translational/rotational landslide, Central Andes, Northwestern ArgentinaAbascal, Liliana del ValleGonzalez Bonorino, GustavoANDESARGENTINALANDSLIDELANDSLIDE HAZARDRISKhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The eastern foothills of the Central Andes, known as the Subandean Ranges, in Peru, Bolivia, and northwestern Argentina, are characterized by heavy rainfall, weakly cemented substrate rocks, thick regoliths, and bedding planes parallel to mountain slopes, features that create serious landslide hazards (Multinational Andean Project: Geoscience for Andean Communities, http://www.pma-map.com). A moderately sized landslide (the Termas Hill landslide) occurred in August 2003 on a slope of the Andean foothills in northwestern Argentina (Figure 1). The slide disrupted regolith and rock, leaving a steepwalled scarp and severing a 130-m-long segment of forest road. The sliding block travelled downslope a few tens of meters, undergoing fragmentation and torsion. On the basis of a topographic survey and structural evidence, this article discusses the geometry and kinematics of the Termas Hill landslide.Fil: Abascal, Liliana del Valle. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Gonzalez Bonorino, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaGeological Society of America2006-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/162086Abascal, Liliana del Valle; Gonzalez Bonorino, Gustavo; Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina; Geological Society of America; Environmental & Engineering Geoscience; 12; 4; 4-2006; 369-3761078-7275CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.2113/gseegeosci.12.4.369info:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/aeg/eeg/article/12/4/369/136769/Kinematics-of-a-Translational-Rotational-Landslideinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:46:40Zoai:ri.conicet.gov.ar:11336/162086instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:46:40.566CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
title Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
spellingShingle Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
Abascal, Liliana del Valle
ANDES
ARGENTINA
LANDSLIDE
LANDSLIDE HAZARD
RISK
title_short Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
title_full Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
title_fullStr Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
title_full_unstemmed Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
title_sort Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina
dc.creator.none.fl_str_mv Abascal, Liliana del Valle
Gonzalez Bonorino, Gustavo
author Abascal, Liliana del Valle
author_facet Abascal, Liliana del Valle
Gonzalez Bonorino, Gustavo
author_role author
author2 Gonzalez Bonorino, Gustavo
author2_role author
dc.subject.none.fl_str_mv ANDES
ARGENTINA
LANDSLIDE
LANDSLIDE HAZARD
RISK
topic ANDES
ARGENTINA
LANDSLIDE
LANDSLIDE HAZARD
RISK
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The eastern foothills of the Central Andes, known as the Subandean Ranges, in Peru, Bolivia, and northwestern Argentina, are characterized by heavy rainfall, weakly cemented substrate rocks, thick regoliths, and bedding planes parallel to mountain slopes, features that create serious landslide hazards (Multinational Andean Project: Geoscience for Andean Communities, http://www.pma-map.com). A moderately sized landslide (the Termas Hill landslide) occurred in August 2003 on a slope of the Andean foothills in northwestern Argentina (Figure 1). The slide disrupted regolith and rock, leaving a steepwalled scarp and severing a 130-m-long segment of forest road. The sliding block travelled downslope a few tens of meters, undergoing fragmentation and torsion. On the basis of a topographic survey and structural evidence, this article discusses the geometry and kinematics of the Termas Hill landslide.
Fil: Abascal, Liliana del Valle. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Gonzalez Bonorino, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
description The eastern foothills of the Central Andes, known as the Subandean Ranges, in Peru, Bolivia, and northwestern Argentina, are characterized by heavy rainfall, weakly cemented substrate rocks, thick regoliths, and bedding planes parallel to mountain slopes, features that create serious landslide hazards (Multinational Andean Project: Geoscience for Andean Communities, http://www.pma-map.com). A moderately sized landslide (the Termas Hill landslide) occurred in August 2003 on a slope of the Andean foothills in northwestern Argentina (Figure 1). The slide disrupted regolith and rock, leaving a steepwalled scarp and severing a 130-m-long segment of forest road. The sliding block travelled downslope a few tens of meters, undergoing fragmentation and torsion. On the basis of a topographic survey and structural evidence, this article discusses the geometry and kinematics of the Termas Hill landslide.
publishDate 2006
dc.date.none.fl_str_mv 2006-04
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/162086
Abascal, Liliana del Valle; Gonzalez Bonorino, Gustavo; Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina; Geological Society of America; Environmental & Engineering Geoscience; 12; 4; 4-2006; 369-376
1078-7275
CONICET Digital
CONICET
url http://hdl.handle.net/11336/162086
identifier_str_mv Abascal, Liliana del Valle; Gonzalez Bonorino, Gustavo; Kinematics of a translational/rotational landslide, Central Andes, Northwestern Argentina; Geological Society of America; Environmental & Engineering Geoscience; 12; 4; 4-2006; 369-376
1078-7275
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.2113/gseegeosci.12.4.369
info:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/aeg/eeg/article/12/4/369/136769/Kinematics-of-a-Translational-Rotational-Landslide
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Geological Society of America
publisher.none.fl_str_mv Geological Society of America
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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