Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.)
- Autores
- Gonzalez Diaz, E.F.; Fauque, L.; Costa, G.; Giaccardp, A.; De Palomera, P.A.; Pereyra, F.
- Año de publicación
- 1997
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The first rock avalanche to be identified in the southern Sierras Pampeanas is described here and its origin analysed. It is located in the northern sector (Cordon El Realito) of the San Luis fault scarp, which marks the western slope of the Sierra Grande de San Luis. It is suggested that the avalanche was triggered by seismic schock, a hypothesis supported by the seismotectonic and geologic conditions of the region as well as by the records of historical seismicity and by the recognition of modern fractures, scarplets and springwater spots in the piedmont area. Several other geological factors also support this suggestion, such as joint density, main shear zone location, attitude of the internal structure of granitoids and other nearby gravitational movements. The primary landforms of the avalanche landscape strongly suggest that the event was a recent one. The estimated speed is about 190 km/hour. © 1997 Asociacón Geológica Argentina.
Fil:Fauque, L. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Costa, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
Fil:Pereyra, F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. - Fuente
- Rev. Asoc. Geol. Argent. 1997;52(1):93-107
- Materia
-
avalanche
rockfall
seismicity
Argentina - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/2.5/ar
- Repositorio
- Institución
- Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
- OAI Identificador
- paperaa:paper_00044822_v52_n1_p93_GonzalezDiaz
Ver los metadatos del registro completo
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Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) Gonzalez Diaz, E.F.Fauque, L.Costa, G.Giaccardp, A.De Palomera, P.A.Pereyra, F.avalancherockfallseismicityArgentinaThe first rock avalanche to be identified in the southern Sierras Pampeanas is described here and its origin analysed. It is located in the northern sector (Cordon El Realito) of the San Luis fault scarp, which marks the western slope of the Sierra Grande de San Luis. It is suggested that the avalanche was triggered by seismic schock, a hypothesis supported by the seismotectonic and geologic conditions of the region as well as by the records of historical seismicity and by the recognition of modern fractures, scarplets and springwater spots in the piedmont area. Several other geological factors also support this suggestion, such as joint density, main shear zone location, attitude of the internal structure of granitoids and other nearby gravitational movements. The primary landforms of the avalanche landscape strongly suggest that the event was a recent one. The estimated speed is about 190 km/hour. © 1997 Asociacón Geológica Argentina.Fil:Fauque, L. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Costa, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.Fil:Pereyra, F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.1997info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://hdl.handle.net/20.500.12110/paper_00044822_v52_n1_p93_GonzalezDiazRev. Asoc. Geol. Argent. 1997;52(1):93-107reponame:Biblioteca Digital (UBA-FCEN)instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesinstacron:UBA-FCENenginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar2025-09-29T13:43:04Zpaperaa:paper_00044822_v52_n1_p93_GonzalezDiazInstitucionalhttps://digital.bl.fcen.uba.ar/Universidad públicaNo correspondehttps://digital.bl.fcen.uba.ar/cgi-bin/oaiserver.cgiana@bl.fcen.uba.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:18962025-09-29 13:43:04.834Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturalesfalse |
dc.title.none.fl_str_mv |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
title |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
spellingShingle |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) Gonzalez Diaz, E.F. avalanche rockfall seismicity Argentina |
title_short |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
title_full |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
title_fullStr |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
title_full_unstemmed |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
title_sort |
Rock avalanche of Potrero de Levés" southern Sierras Pampeanas, Sierra Grande of San Luis, Argentina (32° 30'S lot.) |
dc.creator.none.fl_str_mv |
Gonzalez Diaz, E.F. Fauque, L. Costa, G. Giaccardp, A. De Palomera, P.A. Pereyra, F. |
author |
Gonzalez Diaz, E.F. |
author_facet |
Gonzalez Diaz, E.F. Fauque, L. Costa, G. Giaccardp, A. De Palomera, P.A. Pereyra, F. |
author_role |
author |
author2 |
Fauque, L. Costa, G. Giaccardp, A. De Palomera, P.A. Pereyra, F. |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
avalanche rockfall seismicity Argentina |
topic |
avalanche rockfall seismicity Argentina |
dc.description.none.fl_txt_mv |
The first rock avalanche to be identified in the southern Sierras Pampeanas is described here and its origin analysed. It is located in the northern sector (Cordon El Realito) of the San Luis fault scarp, which marks the western slope of the Sierra Grande de San Luis. It is suggested that the avalanche was triggered by seismic schock, a hypothesis supported by the seismotectonic and geologic conditions of the region as well as by the records of historical seismicity and by the recognition of modern fractures, scarplets and springwater spots in the piedmont area. Several other geological factors also support this suggestion, such as joint density, main shear zone location, attitude of the internal structure of granitoids and other nearby gravitational movements. The primary landforms of the avalanche landscape strongly suggest that the event was a recent one. The estimated speed is about 190 km/hour. © 1997 Asociacón Geológica Argentina. Fil:Fauque, L. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Costa, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Pereyra, F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. |
description |
The first rock avalanche to be identified in the southern Sierras Pampeanas is described here and its origin analysed. It is located in the northern sector (Cordon El Realito) of the San Luis fault scarp, which marks the western slope of the Sierra Grande de San Luis. It is suggested that the avalanche was triggered by seismic schock, a hypothesis supported by the seismotectonic and geologic conditions of the region as well as by the records of historical seismicity and by the recognition of modern fractures, scarplets and springwater spots in the piedmont area. Several other geological factors also support this suggestion, such as joint density, main shear zone location, attitude of the internal structure of granitoids and other nearby gravitational movements. The primary landforms of the avalanche landscape strongly suggest that the event was a recent one. The estimated speed is about 190 km/hour. © 1997 Asociacón Geológica Argentina. |
publishDate |
1997 |
dc.date.none.fl_str_mv |
1997 |
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/20.500.12110/paper_00044822_v52_n1_p93_GonzalezDiaz |
url |
http://hdl.handle.net/20.500.12110/paper_00044822_v52_n1_p93_GonzalezDiaz |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by/2.5/ar |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
Rev. Asoc. Geol. Argent. 1997;52(1):93-107 reponame:Biblioteca Digital (UBA-FCEN) instname:Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales instacron:UBA-FCEN |
reponame_str |
Biblioteca Digital (UBA-FCEN) |
collection |
Biblioteca Digital (UBA-FCEN) |
instname_str |
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales |
instacron_str |
UBA-FCEN |
institution |
UBA-FCEN |
repository.name.fl_str_mv |
Biblioteca Digital (UBA-FCEN) - Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales |
repository.mail.fl_str_mv |
ana@bl.fcen.uba.ar |
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1844618738961219584 |
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12.891075 |