Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño

The drainage basin of Mayo river in the municipalities of San Pablo and La Cruz, Nariño State, is an example of a volcanic shaped filled valley. Doña Juana, Ánimas and Cerro Petacas are volcanoes that have been previously considered as Doña Juana volcanic complex. The geology of the zone is represen...

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Tipo de recurso:
http://purl.org/coar/resource_type/c_6626
Fecha de publicación:
2010
Institución:
Universidad Pedagógica y Tecnológica de Colombia
Repositorio:
RiUPTC: Repositorio Institucional UPTC
Idioma:
spa
OAI Identifier:
oai:repositorio.uptc.edu.co:001/12204
Acceso en línea:
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/3403
https://repositorio.uptc.edu.co/handle/001/12204
Palabra clave:
filled valley
terraces
ash
flows
eruptive epoch
valle relleno
terrazas
ceniza
flujos
época eruptiva
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License
Derechos de autor 2010 Ingeniería Investigación y Desarrollo
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spelling 2010-12-022024-07-05T18:47:46Z2024-07-05T18:47:46Zhttps://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/3403https://repositorio.uptc.edu.co/handle/001/12204The drainage basin of Mayo river in the municipalities of San Pablo and La Cruz, Nariño State, is an example of a volcanic shaped filled valley. Doña Juana, Ánimas and Cerro Petacas are volcanoes that have been previously considered as Doña Juana volcanic complex. The geology of the zone is represented by several units of volcanic origin, which lie on the methasedimentary rocks of Quebradagrande Complex and some hypoabisal igneous bodies. The catchment of Mayo river has been filled with products of these volcanoes, and partially drained out, in several occasions. Volcanic behavior of the complex and specifically the Doña Juana volcano, represented by some deposits of the Mayo river, shows that it had been dominantly of explosive type with some sporadic effusive episodes. The main volumes are constituted by ash and pumice flow, ash and blocks and debris flow deposits, forming in some cases ignimbrites units. With the recollected data until now, an evolutive activity history of the volcanoes complex is proposed. Three eruptive epochs are outlined, which are characterized each of one for presenting many different volcanic deposits with an accumulated thickness of 350m.La cuenca hidrográfica del río Mayo en los municipios de San Pablo y La Cruz, Departamento de Nariño, constituye un ejemplo de un valle relleno por acción volcánica. Doña Juana, Ánimas y Cerro Petacas son volcanes que han sido considerados previamente como el Complejo Volcánico Doña Juana. La geología en la zona está representada por varias unidades de origen volcánico, las cuales reposan sobre las rocas metasedimentarias del Complejo Quebradagrande y algunos cuerpos ígneos hipoabisales. La cuenca del río Mayo ha sido rellenada con los productos de estos volcanes, y parcialmente vaciada, en varias ocasiones. El comportamiento de los volcanes del complejo y específicamente del volcán Doña Juana, representado por algunos de los depósitos de la cuenca del río Mayo, indican que ha sido dominantemente de tipo explosivo con esporádicos episodios efusivos. Los mayores volúmenes están constituidos por depósitos de flujos de ceniza y pómez, de ceniza y bloques y de escombros, que en algunos casos forman, unidades ignimbríticas. Con los datos obtenidos hasta ahora, se propone una historia evolutiva de la actividad de los volcanes del complejo donde se plantean tres épocas eruptivas las cuales se caracterizan por presentar cada una un gran número de diferentes depósitos volcánicos con un espesor total acumulado de350 m.application/pdfspaspaUniversidad Pedagógica y Tecnológica de Colombia - UPTChttps://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/3403/3044Derechos de autor 2010 Ingeniería Investigación y Desarrollohttp://purl.org/coar/access_right/c_abf127http://purl.org/coar/access_right/c_abf2Ingeniería Investigación y Desarrollo; Vol. 10 No. 2: julio-diciembre de 2010; 85-106Ingeniería Investigación y Desarrollo; Vol. 10 Núm. 2: julio-diciembre de 2010; 85-1062422-43241900-771Xfilled valleyterracesashflowseruptive epochvalle rellenoterrazascenizaflujosépoca eruptivaStratigraphy of the volcanic deposits in the high catchment of mayo river, department of NariñoEstratigrafía de los depósitos volcánicos en la cuenca alta del río Mayo, departamento de Nariñoinfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6626http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a210http://purl.org/coar/version/c_970fb48d4fbd8a85Naranjo-Henao, José LuisPulgarín-Alzate, Bernardo AlonsoNarváez-Marulanda, Blanca Liliana001/12204oai:repositorio.uptc.edu.co:001/122042025-07-18 11:25:46.237metadata.onlyhttps://repositorio.uptc.edu.coRepositorio Institucional UPTCrepositorio.uptc@uptc.edu.co
dc.title.en-US.fl_str_mv Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
dc.title.es-ES.fl_str_mv Estratigrafía de los depósitos volcánicos en la cuenca alta del río Mayo, departamento de Nariño
title Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
spellingShingle Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
filled valley
terraces
ash
flows
eruptive epoch
valle relleno
terrazas
ceniza
flujos
época eruptiva
title_short Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
title_full Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
title_fullStr Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
title_full_unstemmed Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
title_sort Stratigraphy of the volcanic deposits in the high catchment of mayo river, department of Nariño
dc.subject.en-US.fl_str_mv filled valley
terraces
ash
flows
eruptive epoch
topic filled valley
terraces
ash
flows
eruptive epoch
valle relleno
terrazas
ceniza
flujos
época eruptiva
dc.subject.es-ES.fl_str_mv valle relleno
terrazas
ceniza
flujos
época eruptiva
description The drainage basin of Mayo river in the municipalities of San Pablo and La Cruz, Nariño State, is an example of a volcanic shaped filled valley. Doña Juana, Ánimas and Cerro Petacas are volcanoes that have been previously considered as Doña Juana volcanic complex. The geology of the zone is represented by several units of volcanic origin, which lie on the methasedimentary rocks of Quebradagrande Complex and some hypoabisal igneous bodies. The catchment of Mayo river has been filled with products of these volcanoes, and partially drained out, in several occasions. Volcanic behavior of the complex and specifically the Doña Juana volcano, represented by some deposits of the Mayo river, shows that it had been dominantly of explosive type with some sporadic effusive episodes. The main volumes are constituted by ash and pumice flow, ash and blocks and debris flow deposits, forming in some cases ignimbrites units. With the recollected data until now, an evolutive activity history of the volcanoes complex is proposed. Three eruptive epochs are outlined, which are characterized each of one for presenting many different volcanic deposits with an accumulated thickness of 350m.
publishDate 2010
dc.date.accessioned.none.fl_str_mv 2024-07-05T18:47:46Z
dc.date.available.none.fl_str_mv 2024-07-05T18:47:46Z
dc.date.none.fl_str_mv 2010-12-02
dc.type.none.fl_str_mv info:eu-repo/semantics/article
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.coarversion.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_6626
dc.type.coarversion.spa.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a210
format http://purl.org/coar/resource_type/c_6626
dc.identifier.none.fl_str_mv https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/3403
dc.identifier.uri.none.fl_str_mv https://repositorio.uptc.edu.co/handle/001/12204
url https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/3403
https://repositorio.uptc.edu.co/handle/001/12204
dc.language.none.fl_str_mv spa
dc.language.iso.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/3403/3044
dc.rights.es-ES.fl_str_mv Derechos de autor 2010 Ingeniería Investigación y Desarrollo
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.coar.spa.fl_str_mv http://purl.org/coar/access_right/c_abf127
rights_invalid_str_mv Derechos de autor 2010 Ingeniería Investigación y Desarrollo
http://purl.org/coar/access_right/c_abf127
http://purl.org/coar/access_right/c_abf2
dc.format.none.fl_str_mv application/pdf
dc.publisher.es-ES.fl_str_mv Universidad Pedagógica y Tecnológica de Colombia - UPTC
dc.source.en-US.fl_str_mv Ingeniería Investigación y Desarrollo; Vol. 10 No. 2: julio-diciembre de 2010; 85-106
dc.source.es-ES.fl_str_mv Ingeniería Investigación y Desarrollo; Vol. 10 Núm. 2: julio-diciembre de 2010; 85-106
dc.source.none.fl_str_mv 2422-4324
1900-771X
institution Universidad Pedagógica y Tecnológica de Colombia
repository.name.fl_str_mv Repositorio Institucional UPTC
repository.mail.fl_str_mv repositorio.uptc@uptc.edu.co
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