Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú
Descripción del Articulo
Páginas 467-473. | Trabajo presentado en The International Conference on Landslide Risk Management, realizado en Vancouver, Canada, de 31 mayo a 3 junio, 2005.
| Autores: | , , , , , |
|---|---|
| Formato: | objeto de conferencia |
| Fecha de Publicación: | 2005 |
| Institución: | Instituto Geológico, Minero y Metalúrgico |
| Repositorio: | INGEMMET-Institucional |
| Lenguaje: | inglés |
| OAI Identifier: | oai:repositorio.ingemmet.gob.pe:20.500.12544/2078 |
| Enlace del recurso: | https://hdl.handle.net/20.500.12544/2078 https://doi.org/10.1201/9781439833711 |
| Nivel de acceso: | acceso abierto |
| Materia: | Peligros geológicos Flujo de detritos Inundaciones Debris flows Geological hazards Floods |
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| dc.title.es_PE.fl_str_mv |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| title |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| spellingShingle |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú Fidel Smoll, Lionel Peligros geológicos Flujo de detritos Inundaciones Debris flows Geological hazards Floods |
| title_short |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| title_full |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| title_fullStr |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| title_full_unstemmed |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| title_sort |
Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú |
| author |
Fidel Smoll, Lionel |
| author_facet |
Fidel Smoll, Lionel Guzmán Martínez, Antonio Zegarra Loo, Juan Vílchez Mata, Manuel Salomón Colque Tula, Julio Jackson, L.E., Jr. |
| author_role |
author |
| author2 |
Guzmán Martínez, Antonio Zegarra Loo, Juan Vílchez Mata, Manuel Salomón Colque Tula, Julio Jackson, L.E., Jr. |
| author2_role |
author author author author author |
| dc.contributor.author.fl_str_mv |
Fidel Smoll, Lionel Guzmán Martínez, Antonio Zegarra Loo, Juan Vílchez Mata, Manuel Salomón Colque Tula, Julio Jackson, L.E., Jr. |
| dc.subject.es_PE.fl_str_mv |
Peligros geológicos Flujo de detritos Inundaciones Debris flows Geological hazards Floods |
| topic |
Peligros geológicos Flujo de detritos Inundaciones Debris flows Geological hazards Floods |
| description |
Páginas 467-473. | Trabajo presentado en The International Conference on Landslide Risk Management, realizado en Vancouver, Canada, de 31 mayo a 3 junio, 2005. |
| publishDate |
2005 |
| dc.date.accessioned.none.fl_str_mv |
2019-06-07T22:50:12Z |
| dc.date.available.none.fl_str_mv |
2019-06-07T22:50:12Z |
| dc.date.issued.fl_str_mv |
2005-06 |
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info:eu-repo/semantics/conferenceObject |
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conferenceObject |
| dc.identifier.citation.es_PE.fl_str_mv |
Fídel, L.; Guzmán, A.; Zegarra, J.; Vílchez, M.; Colque, J. & Jackson, L.E., Jr. (2005). Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú. In: Landslide Risk Management. London: Taylor & Francis, p. 467-473. DOI: 10.1201/9781439833711 |
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urn:isbn:041538 043X |
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https://hdl.handle.net/20.500.12544/2078 |
| dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.1201/9781439833711 |
| dc.identifier.bibliographicCitation.es_PE.fl_str_mv |
Landslide Risk Management.London, 2005. |
| identifier_str_mv |
Fídel, L.; Guzmán, A.; Zegarra, J.; Vílchez, M.; Colque, J. & Jackson, L.E., Jr. (2005). Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú. In: Landslide Risk Management. London: Taylor & Francis, p. 467-473. DOI: 10.1201/9781439833711 urn:isbn:041538 043X Landslide Risk Management.London, 2005. |
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https://hdl.handle.net/20.500.12544/2078 https://doi.org/10.1201/9781439833711 |
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eng |
| language |
eng |
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info:eu-repo/semantics/openAccess |
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https://creativecommons.org/licenses/by-nc-sa/4.0/ |
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openAccess |
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https://creativecommons.org/licenses/by-nc-sa/4.0/ |
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application/pdf |
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Matucana Huarochirí Perú Río Rímac |
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Taylor & Francis |
| dc.publisher.country.es_PE.fl_str_mv |
GB |
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Instituto Geológico, Minero y Metalúrgico – INGEMMET Repositorio Institucional INGEMMET |
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Fidel Smoll, LionelGuzmán Martínez, AntonioZegarra Loo, JuanVílchez Mata, Manuel SalomónColque Tula, JulioJackson, L.E., Jr.MatucanaHuarochiríPerúRío Rímac2019-06-07T22:50:12Z2019-06-07T22:50:12Z2005-06Fídel, L.; Guzmán, A.; Zegarra, J.; Vílchez, M.; Colque, J. & Jackson, L.E., Jr. (2005). Investigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perú. In: Landslide Risk Management. London: Taylor & Francis, p. 467-473. DOI: 10.1201/9781439833711urn:isbn:041538 043Xhttps://hdl.handle.net/20.500.12544/2078https://doi.org/10.1201/9781439833711Landslide Risk Management.London, 2005.Páginas 467-473. | Trabajo presentado en The International Conference on Landslide Risk Management, realizado en Vancouver, Canada, de 31 mayo a 3 junio, 2005.The small city of Matucana (population 5800), Province of Huarochirí, Perú is located on the flood plain of Rimac River in Andes Occidental, approximately 75 km east of Lima at an elevation of 2390 m (area of 11° 50.489’ S, 76° 22.857’ W). Adjacent ridges and mountain peaks rise to 5000 m. Matucana shares a 300m wide valley bottom with two transportation arteries: Carretera Central, the only highway in Perú connecting the Amazon basin to the Pacific Coast and Ferrocarril Central, the highest standard gauge railway in the world which services mines and communities in the Andes. The present course of Rimac River is controlled by a dike and fill for the highway and railroad. These structures confine it to the northern portion of its flood plain. Consequently, parts of Matucana are lower in elevation than the bed of Rimac River. Payhua Creek (PC), a steep, debris-flow-prone tributary to Rimac River, has built an extensive fan at the upstream end of the city. Debris flows from PC has dammed Rimac River and diverted it into Matucana. This type of disaster occurred 1959 and 1983 when heavy precipitation occurred in the normally arid Andes Occidental. The 1959 event was particularly notable as it destroyed 90% of Matucana with loss of life. Although these events were not well documented, investigation of the PC fan and documentation of 1983 deposits on the fan indicate that the 1983 debris flow had a volume in the 0.12 106 to 106m3 range. Investigation of surficial and bedrock geology including mapping of all landslides in PC basin was carried out in 2004. A landslide complex immediately west of Payhua village is the most significant source of debris flow sediment in the basin. Incision of an unfavourable succession of andesite flows overlying a pervasively fractured tuff is responsible for the concentration of landslides in the Payhua village area. The area affected by landsliding in this area has increased by a factor of five since 1951. The PC basin upstream from Payhua has been a relatively small source of debris flows during the past 600 to 800 years based upon archaeological evidence. Exposures of debris flow deposits in the PC fan indicate that debris flow events larger than those of 1959 and 1983 have occurred in the recent geologic past. Matucana has also grown significantly since 1983 and has further encroached on the Rimac River flood plain and the PC fan. As a result, if debris flows of the magnitude of those in 1959 and 1983 occur, direct burial of the upstream area of Matucana by debris flows is likely.application/pdfengTaylor & FrancisGBinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/Instituto Geológico, Minero y Metalúrgico – INGEMMETRepositorio Institucional INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETPeligros geológicosFlujo de detritosInundacionesDebris flowsGeological hazardsFloodsInvestigation of the origin and magnitude of debris flows from the Payhua Creek basin, Matucana area, Huarochirí Province, Perúinfo:eu-repo/semantics/conferenceObjectGeologíaORIGINALFidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdfFidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdfArtículo presentado en congresoapplication/pdf460432https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2078/1/Fidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdfe54916b79b146d0a5122d69be57b24aeMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2078/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52TEXTFidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdf.txtFidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdf.txtExtracted texttext/plain28155https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2078/3/Fidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdf.txtb0d756ecfe7c6f889c0d5c26992a836aMD53THUMBNAILFidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdf.jpgFidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdf.jpgGenerated Thumbnailimage/jpeg21488https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/2078/4/Fidel-Investigation_of_the_origin_and_magnitude...Huarochiri.pdf.jpgf06f5ce042cf39f16959cddda3000878MD5420.500.12544/2078oai:repositorio.ingemmet.gob.pe:20.500.12544/20782021-10-06 15:38:29.919Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.peTGljZW5jaWEgZGUgVXNvCgpFbCBJbnN0aXR1dG8gR2VvbMOzZ2ljbywgTWluZXJvIHkgTWV0YWzDunJnaWNvIOKAkyBJTkdFTU1FVCwgZGlmdW5kZSBtZWRpYW50ZSBzdSByZXBvc2l0b3JpbyBsYSBwcm9kdWNjacOzbiBjaWVudMOtZmljYSB5IHTDqWNuaWNhIHByb2R1Y2lkYSBwb3IgbG9zIG1pZW1icm9zIGRlIGxhIGluc3RpdHVjacOzbi4gRWwgY29udGVuaWRvIGRlIGxvcyBkb2N1bWVudG9zIGRpZ2l0YWxlcyBlcyBkZSBhY2Nlc28gYWJpZXJ0byBwYXJhIHRvZGEgcGVyc29uYSBpbnRlcmVzYWRhLgoKU2UgYWNlcHRhIGxhIGRpZnVzacOzbiBww7pibGljYSBkZSBsYSBvYnJhLCBzdSBjb3BpYSB5IHJlcHJvZHVjacOzbi4gUGFyYSBlbGxvIGVzIG5lY2VzYXJpbyBxdWUgc2UgY3VtcGxhIGNvbiBsYXMgc2lndWllbnRlcyBjb25kaWNpb25lczoKLSBFbCBuZWNlc2FyaW8gcmVjb25vY2ltaWVudG8gZGUgbGEgYXV0b3LDrWEgZGUgbGEgb2JyYSwgaWRlbnRpZmljYW5kbyBvcG9ydHVuYSB5IGNvcnJlY3RhbWVudGUgYSBsYSBwZXJzb25hIHF1ZSBwb3NlYSBsb3MgZGVyZWNob3MgZGUgYXV0b3IuCi0gTm8gZXN0w6EgcGVybWl0aWRvIGVsIHVzbyBpbmRlYmlkbyBkZSBsYSBvYnJhIGNvbiBmaW5lcyBkZSBsdWNybyBvIGN1YWxxdWllciB0aXBvIGRlIGFjdGl2aWRhZCBxdWUgcHJvZHV6Y2EgZ2FuYW5jaWFzIGEgbGFzIHBlcnNvbmFzIHF1ZSBsbyBkaWZ1bmRlbiBzaW4gZWwgY29uc2VudGltaWVudG8gZGVsIGF1dG9yLgotIExvcyB0cmFiYWpvcyBxdWUgc2UgcHJvZHV6Y2FuIGEgcGFydGlyIGRlIGxhIG9icmEgZGViZW4gcG9zZWVyIGxhIGNpdGFjacOzbiBwZXJ0aW5lbnRlIGRlIGFjdWVyZG8gYSBjdWFscXVpZXJhIGRlIGxvcyBlc3RpbG9zIChBUEEsIElTTywgVmFuY3V2ZXIsIGV0YykgZWxlZ2lkb3MgcGFyYSBsYSByZWRhY2Npw7NuIGRlIGxhcyByZWZlcmVuY2lhcyBiaWJsaW9ncsOhZmljYXMuIENhc28gY29udHJhcmlvIHNlIGluY3Vycmlyw6EgZW4gbGEgZmlndXJhIGp1csOtZGljYSBkZWwgcGxhZ2lvLgoKTG9zIGRlcmVjaG9zIG1vcmFsZXMgZGVsIGF1dG9yIG5vIHNvbiBhZmVjdGFkb3MgcG9yIGxhIHByZXNlbnRlIGxpY2VuY2lhIGRlIHVzby4KCkRlcmVjaG9zIGRlIGF1dG9yCgpMb3MgZGVyZWNob3MgZGUgYXV0b3Igc2UgZW5jdWVudHJhbiBwcm90ZWdpZG9zIHBvciBsYSBsZWdpc2xhY2nDs24gcGVydWFuYTogTGV5IHNvYnJlIGVsIERlcmVjaG8gZGUgQXV0b3IgcHJvbXVsZ2FkbyBlbiAxOTk2IChELkwuIE7CsCA4MjIpLCBMZXkgcXVlIG1vZGlmaWNhIGxvcyBhcnTDrWN1bG9zIDE4OMKweSAxODnCsCBkZWwgZGVjcmV0byBsZWdpc2xhdGl2byBOwrAgODIyLCBMZXkgc29icmUgRGVyZWNob3MgZGUgQXV0b3IgcHJvbXVsZ2FkYSBlbiAyMDA1IChMZXkgTsKwIDI4NTE3KSwgRGVjcmV0byBMZWdpc2xhdGl2byBxdWUgYXBydWViYSBsYSBtb2RpZmljYWNpw7NuIGRlbCBEZWNyZXRvIExlZ2lzbGF0aXZvIE7CsCA4MjIsIExleSBzb2JyZSBlbCBEZXJlY2hvIGRlIEF1dG9yIHByb211bGdhZG8gZW4gMjAwOCAoRC5MLiBOwrAgMTA3NikuCg== |
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Nota importante:
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
