Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru)
Descripción del Articulo
A network of air and ground temperature sensors installed 2004-2014 has enabled the discovery of permafrost on the Coropuna (6377 m) and Chachani (6057 m) volcanoes. However, on the Misti (5820 m) volcano there is no permafrost, which can be attributed to geothermal heat. Misti and Chachani are very...
Autores: | , , , , , , , , , , |
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Formato: | objeto de conferencia |
Fecha de Publicación: | 2015 |
Institución: | Instituto Geológico, Minero y Metalúrgico |
Repositorio: | INGEMMET-Institucional |
Lenguaje: | inglés |
OAI Identifier: | oai:repositorio.ingemmet.gob.pe:20.500.12544/4391 |
Enlace del recurso: | https://hdl.handle.net/20.500.12544/4391 |
Nivel de acceso: | acceso abierto |
Materia: | Volcanes Geofísica Permafrost Sensores remotos http://purl.org/pe-repo/ocde/ford#1.05.00 http://purl.org/pe-repo/ocde/ford#1.05.06 http://purl.org/pe-repo/ocde/ford#1.05.07 |
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dc.title.es_PE.fl_str_mv |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
title |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
spellingShingle |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) Úbeda Palenque, José Volcanes Geofísica Permafrost Sensores remotos http://purl.org/pe-repo/ocde/ford#1.05.00 http://purl.org/pe-repo/ocde/ford#1.05.06 http://purl.org/pe-repo/ocde/ford#1.05.07 |
title_short |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
title_full |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
title_fullStr |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
title_full_unstemmed |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
title_sort |
Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru) |
author |
Úbeda Palenque, José |
author_facet |
Úbeda Palenque, José Yoshikawa, Kenji Pari Pinto, Walter Palacios Estremera, David Macias, Pablo Apaza Choquehuayta, Fredy Erlingtton Ccallata Pacsi, Beto Miranda Cruz, Rafael Concha Niño de Guzmán, Ronald Fernando Vásquez Choque, Estibene Pool Cruz, Rolando |
author_role |
author |
author2 |
Yoshikawa, Kenji Pari Pinto, Walter Palacios Estremera, David Macias, Pablo Apaza Choquehuayta, Fredy Erlingtton Ccallata Pacsi, Beto Miranda Cruz, Rafael Concha Niño de Guzmán, Ronald Fernando Vásquez Choque, Estibene Pool Cruz, Rolando |
author2_role |
author author author author author author author author author author |
dc.contributor.author.fl_str_mv |
Úbeda Palenque, José Yoshikawa, Kenji Pari Pinto, Walter Palacios Estremera, David Macias, Pablo Apaza Choquehuayta, Fredy Erlingtton Ccallata Pacsi, Beto Miranda Cruz, Rafael Concha Niño de Guzmán, Ronald Fernando Vásquez Choque, Estibene Pool Cruz, Rolando |
dc.subject.es_PE.fl_str_mv |
Volcanes Geofísica Permafrost Sensores remotos |
topic |
Volcanes Geofísica Permafrost Sensores remotos http://purl.org/pe-repo/ocde/ford#1.05.00 http://purl.org/pe-repo/ocde/ford#1.05.06 http://purl.org/pe-repo/ocde/ford#1.05.07 |
dc.subject.ocde.es_PE.fl_str_mv |
http://purl.org/pe-repo/ocde/ford#1.05.00 http://purl.org/pe-repo/ocde/ford#1.05.06 http://purl.org/pe-repo/ocde/ford#1.05.07 |
description |
A network of air and ground temperature sensors installed 2004-2014 has enabled the discovery of permafrost on the Coropuna (6377 m) and Chachani (6057 m) volcanoes. However, on the Misti (5820 m) volcano there is no permafrost, which can be attributed to geothermal heat. Misti and Chachani are very close to each other, near the city of Arequipa (S. Peru). Coropuna is 150 km to the west. Various volcanic eruptions have taken place on Misti and Coropuna in the last 10 ka (Úbeda et al, 2012). The volcanic activity on the Chachani seems to be much older, although it has not been researched to date. Coropuna is covered by a glacial system of _40 km2 (23-11-2013) and the moraines surrounding the volcanic complex indicate a surface of >500 km2 >10 ka ago (Úbeda et al, 2011). On Chachani the evidence also suggests a great extent in the past although in this case there are no glaciers conserved at the present day. On Misti there are currently no glaciers either, nor is there any evidence conserved of their earlier presence, and this has also been related to geothermal heat. As well as other study areas, the CRYOPERU sensor network includes 4 stations in the sector Coropuna-NE; 3 stations in Coropuna-SE; 3 stations in Chachani-SE and 3 stations in Misti-NW. The stations are at different altitudes, in an interval of 4300-6000 m. Each station has a thermometer to measure the air temperature (at a height of 0.50 m) and three thermometers to measure the ground temperature (at depths of 0.15, 0.30 and 1.00 m). The sensors are synchronized in GPS time and record the temperature every 30 minutes. |
publishDate |
2015 |
dc.date.accessioned.none.fl_str_mv |
2023-02-22T15:28:58Z |
dc.date.available.none.fl_str_mv |
2023-02-22T15:28:58Z |
dc.date.issued.fl_str_mv |
2015 |
dc.type.es_PE.fl_str_mv |
info:eu-repo/semantics/conferenceObject |
dc.type.version.es_PE.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
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conferenceObject |
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dc.identifier.citation.es_PE.fl_str_mv |
Úbeda, J., Yoshikawa, K., Pari, W., Palacios, D., Macias, P., Apaza, F., Ccallata, B., Miranda, R., Concha, R., Vásquez, Estibene P. & Cruz, R. (2015). Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru). Geophysical Research Abstracts, 17. |
dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/20.500.12544/4391 |
dc.identifier.bibliographicCitation.es_PE.fl_str_mv |
Geophysical Research Abstracts, vol.17, 2015, p.EGU2015-12592-2. |
identifier_str_mv |
Úbeda, J., Yoshikawa, K., Pari, W., Palacios, D., Macias, P., Apaza, F., Ccallata, B., Miranda, R., Concha, R., Vásquez, Estibene P. & Cruz, R. (2015). Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru). Geophysical Research Abstracts, 17. Geophysical Research Abstracts, vol.17, 2015, p.EGU2015-12592-2. |
url |
https://hdl.handle.net/20.500.12544/4391 |
dc.language.iso.es_PE.fl_str_mv |
eng |
language |
eng |
dc.relation.conference.es_PE.fl_str_mv |
Trabajo presentado en el European Geophysical Union, General Assembly, Vienna, Austria, 12-17 abril, 2015 |
dc.rights.es_PE.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.uri.es_PE.fl_str_mv |
https://creativecommons.org/licenses/by-nc-sa/4.0/deed.es |
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openAccess |
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https://creativecommons.org/licenses/by-nc-sa/4.0/deed.es |
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dc.coverage.spatial.es_PE.fl_str_mv |
Volcán Coropuna Volcán Chachani Arequipa Perú |
dc.publisher.es_PE.fl_str_mv |
Copernicus |
dc.source.es_PE.fl_str_mv |
Repositorio Institucional INGEMMET Instituto Geológico, Minero y Metalúrgico – INGEMMET |
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Úbeda Palenque, JoséYoshikawa, KenjiPari Pinto, WalterPalacios Estremera, DavidMacias, PabloApaza Choquehuayta, Fredy ErlingttonCcallata Pacsi, BetoMiranda Cruz, RafaelConcha Niño de Guzmán, Ronald FernandoVásquez Choque, Estibene PoolCruz, RolandoVolcán CoropunaVolcán ChachaniArequipaPerú2023-02-22T15:28:58Z2023-02-22T15:28:58Z2015Úbeda, J., Yoshikawa, K., Pari, W., Palacios, D., Macias, P., Apaza, F., Ccallata, B., Miranda, R., Concha, R., Vásquez, Estibene P. & Cruz, R. (2015). Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru). Geophysical Research Abstracts, 17.https://hdl.handle.net/20.500.12544/4391Geophysical Research Abstracts, vol.17, 2015, p.EGU2015-12592-2.A network of air and ground temperature sensors installed 2004-2014 has enabled the discovery of permafrost on the Coropuna (6377 m) and Chachani (6057 m) volcanoes. However, on the Misti (5820 m) volcano there is no permafrost, which can be attributed to geothermal heat. Misti and Chachani are very close to each other, near the city of Arequipa (S. Peru). Coropuna is 150 km to the west. Various volcanic eruptions have taken place on Misti and Coropuna in the last 10 ka (Úbeda et al, 2012). The volcanic activity on the Chachani seems to be much older, although it has not been researched to date. Coropuna is covered by a glacial system of _40 km2 (23-11-2013) and the moraines surrounding the volcanic complex indicate a surface of >500 km2 >10 ka ago (Úbeda et al, 2011). On Chachani the evidence also suggests a great extent in the past although in this case there are no glaciers conserved at the present day. On Misti there are currently no glaciers either, nor is there any evidence conserved of their earlier presence, and this has also been related to geothermal heat. As well as other study areas, the CRYOPERU sensor network includes 4 stations in the sector Coropuna-NE; 3 stations in Coropuna-SE; 3 stations in Chachani-SE and 3 stations in Misti-NW. The stations are at different altitudes, in an interval of 4300-6000 m. Each station has a thermometer to measure the air temperature (at a height of 0.50 m) and three thermometers to measure the ground temperature (at depths of 0.15, 0.30 and 1.00 m). The sensors are synchronized in GPS time and record the temperature every 30 minutes.application/pdf1 páginasengCopernicusinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/deed.esRepositorio Institucional INGEMMETInstituto Geológico, Minero y Metalúrgico – INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETVolcanesGeofísicaPermafrostSensores remotoshttp://purl.org/pe-repo/ocde/ford#1.05.00http://purl.org/pe-repo/ocde/ford#1.05.06http://purl.org/pe-repo/ocde/ford#1.05.07Geophysical surveys on permafrost in Coropuna and Chachani volcanoes (southern Peru)info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionTrabajo presentado en el European Geophysical Union, General Assembly, Vienna, Austria, 12-17 abril, 2015LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/4391/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52ORIGINALUbeda-Geophysical_surveys_permafrost_Coropuna.pdfUbeda-Geophysical_surveys_permafrost_Coropuna.pdfapplication/pdf42032https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/4391/1/Ubeda-Geophysical_surveys_permafrost_Coropuna.pdfa5adbbea00de2c6d6d48fc962f30b04fMD51TEXTUbeda-Geophysical_surveys_permafrost_Coropuna.pdf.txtUbeda-Geophysical_surveys_permafrost_Coropuna.pdf.txtExtracted texttext/plain2982https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/4391/3/Ubeda-Geophysical_surveys_permafrost_Coropuna.pdf.txtd3908d623b6a92d09bfa6910d091f600MD53THUMBNAILUbeda-Geophysical_surveys_permafrost_Coropuna.pdf.jpgUbeda-Geophysical_surveys_permafrost_Coropuna.pdf.jpgGenerated Thumbnailimage/jpeg18187https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/4391/4/Ubeda-Geophysical_surveys_permafrost_Coropuna.pdf.jpge128d33cc478e5b9c38f6f4591de8d3aMD5420.500.12544/4391oai:repositorio.ingemmet.gob.pe:20.500.12544/43912023-02-22 11:16:14.492Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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 |
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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).