Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)

The photointerpretation, using aerial photographs recorded from the Armero's Debris Flow, few days after it took place, in agreement with survivors reports, indicate that the event occurred in three principal pulses, each one with different hydrodynamic characteristics, as has been observed in...

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Autores:
Ujueta L., Guillermo
Mojica, Jairo
Tipo de recurso:
Article of journal
Fecha de publicación:
1995
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/41892
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/41892
http://bdigital.unal.edu.co/31989/
Palabra clave:
Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
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repository_id_str
spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Ujueta L., Guillermo11483135-158d-469d-b41d-9516bedebfe2300Mojica, Jairo60c8ebaa-ce0a-458a-891e-31533e14796c3002019-06-28T10:20:52Z2019-06-28T10:20:52Z1995https://repositorio.unal.edu.co/handle/unal/41892http://bdigital.unal.edu.co/31989/The photointerpretation, using aerial photographs recorded from the Armero's Debris Flow, few days after it took place, in agreement with survivors reports, indicate that the event occurred in three principal pulses, each one with different hydrodynamic characteristics, as has been observed in other places of the world. In the first place there was a preceding muddy flow that only affected the shallower places such as the closer ones to the Lagunilla River; the first pulse was an extremely dense flow supersatured with solids with a variable and relatively low velocity that resulted in a continous debris sheet that covered the flat lands with a thickness of up to 3 meters height and a radius of 2.5 km. The push and advance of this flow which included the biggest blocks was the responsible of the destruction of Armero. The effect of this flow was differential, as in higher zones the debris flow did not demolish houses and was inyected though doors and windows. The high density of this flow was one of the main reasons that it did not affect some streets with high slopes.  The second pulse consisted of high velocity turbulent running water, loaded with pebbles and gravels, which generated a high erosion capacity that stripped off the former fan, providing a terrace aspect and producing new distributary water channels. The third pulse was a low level water flow with a high concentration of gravel, sand and mud, which took place for several hours. It was concluded, from the photointerpretation, that the Armero's Debris Row according to its hydrodynamic characteristics, reached the flatter topography and overflowed the Lagunilla's riverbed at different places.application/pdfspaDepartamento de Geocienciashttp://revistas.unal.edu.co/index.php/geocol/article/view/31323Universidad Nacional de Colombia Revistas electrónicas UN Geología ColombianaGeología ColombianaGeología Colombiana - An International Journal on Geosciences; Vol. 19 (1995); 5-20 Geología Colombiana; Vol. 19 (1995); 5-20 2357-3767 0072-0992Ujueta L., Guillermo and Mojica, Jairo (1995) Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia). Geología Colombiana - An International Journal on Geosciences; Vol. 19 (1995); 5-20 Geología Colombiana; Vol. 19 (1995); 5-20 2357-3767 0072-0992 .Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)Artículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTGeologíaCiencias de la tierraGeocienciasLlanura de ArmeroFotointerpretaciónflujos de escombrosSistema fluvial Lagunilla-AzufradopulsosGeologíaCiencias de la tierraGeocienciasLlanura de ArmeroFotointerpretaciónflujos de escombrosSistema fluvial Lagunilla-AzufradopulsosORIGINAL31323-113450-1-PB.pdfapplication/pdf18102006https://repositorio.unal.edu.co/bitstream/unal/41892/1/31323-113450-1-PB.pdf60eecc44b6cc4792a27aa0413511f95dMD51THUMBNAIL31323-113450-1-PB.pdf.jpg31323-113450-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg12049https://repositorio.unal.edu.co/bitstream/unal/41892/2/31323-113450-1-PB.pdf.jpg077d0de004ae9616709f5c3cdd464d80MD52unal/41892oai:repositorio.unal.edu.co:unal/418922024-02-02 23:06:25.416Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co
dc.title.spa.fl_str_mv Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
title Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
spellingShingle Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
title_short Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
title_full Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
title_fullStr Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
title_full_unstemmed Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
title_sort Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia)
dc.creator.fl_str_mv Ujueta L., Guillermo
Mojica, Jairo
dc.contributor.author.spa.fl_str_mv Ujueta L., Guillermo
Mojica, Jairo
dc.subject.proposal.spa.fl_str_mv Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
topic Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
Geología
Ciencias de la tierra
Geociencias
Llanura de Armero
Fotointerpretación
flujos de escombros
Sistema fluvial Lagunilla-Azufrado
pulsos
description The photointerpretation, using aerial photographs recorded from the Armero's Debris Flow, few days after it took place, in agreement with survivors reports, indicate that the event occurred in three principal pulses, each one with different hydrodynamic characteristics, as has been observed in other places of the world. In the first place there was a preceding muddy flow that only affected the shallower places such as the closer ones to the Lagunilla River; the first pulse was an extremely dense flow supersatured with solids with a variable and relatively low velocity that resulted in a continous debris sheet that covered the flat lands with a thickness of up to 3 meters height and a radius of 2.5 km. The push and advance of this flow which included the biggest blocks was the responsible of the destruction of Armero. The effect of this flow was differential, as in higher zones the debris flow did not demolish houses and was inyected though doors and windows. The high density of this flow was one of the main reasons that it did not affect some streets with high slopes.  The second pulse consisted of high velocity turbulent running water, loaded with pebbles and gravels, which generated a high erosion capacity that stripped off the former fan, providing a terrace aspect and producing new distributary water channels. The third pulse was a low level water flow with a high concentration of gravel, sand and mud, which took place for several hours. It was concluded, from the photointerpretation, that the Armero's Debris Row according to its hydrodynamic characteristics, reached the flatter topography and overflowed the Lagunilla's riverbed at different places.
publishDate 1995
dc.date.issued.spa.fl_str_mv 1995
dc.date.accessioned.spa.fl_str_mv 2019-06-28T10:20:52Z
dc.date.available.spa.fl_str_mv 2019-06-28T10:20:52Z
dc.type.spa.fl_str_mv Artículo de revista
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dc.type.content.spa.fl_str_mv Text
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format http://purl.org/coar/resource_type/c_6501
status_str publishedVersion
dc.identifier.uri.none.fl_str_mv https://repositorio.unal.edu.co/handle/unal/41892
dc.identifier.eprints.spa.fl_str_mv http://bdigital.unal.edu.co/31989/
url https://repositorio.unal.edu.co/handle/unal/41892
http://bdigital.unal.edu.co/31989/
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language spa
dc.relation.spa.fl_str_mv http://revistas.unal.edu.co/index.php/geocol/article/view/31323
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Geología Colombiana
Geología Colombiana
dc.relation.ispartofseries.none.fl_str_mv Geología Colombiana - An International Journal on Geosciences; Vol. 19 (1995); 5-20 Geología Colombiana; Vol. 19 (1995); 5-20 2357-3767 0072-0992
dc.relation.references.spa.fl_str_mv Ujueta L., Guillermo and Mojica, Jairo (1995) Fotointerpretación y observaciones de campo del flujo de escombros de noviembre 13 de 1985 en armero (tolima, colombia). Geología Colombiana - An International Journal on Geosciences; Vol. 19 (1995); 5-20 Geología Colombiana; Vol. 19 (1995); 5-20 2357-3767 0072-0992 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
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dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
Derechos reservados - Universidad Nacional de Colombia
http://creativecommons.org/licenses/by-nc/4.0/
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.format.mimetype.spa.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv Departamento de Geociencias
institution Universidad Nacional de Colombia
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