The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results
The rock glaciers of the Andes of Santiago de Chile are unsuspicious, but important water resources and play a key role within the debris transport system of this semiarid high mountain area. The significance of these bodies of debris and ice within the geomorphologic and hydrologic system is shown...
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Pontificia Universidad Católica de Chile, Facultad de Historia, Geografía y Ciencias Políticas, Instituto de Geografía
2021
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Online Access: | https://ojs.uc.cl/index.php/RGNG/article/view/42865 |
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ftpunivcchileojs:oai:ojs2.ojs.uc.cl:article/42865 2023-06-06T11:54:44+02:00 The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results La Importancia de los Glaciares de Escombros en los Sistemas Geomorfológico e Hidrológico de la Cordillera de Santiago: Fundamentos y Primeros Resultados BRENNING, ALEXANDER 2021-10-18 application/pdf https://ojs.uc.cl/index.php/RGNG/article/view/42865 spa spa Pontificia Universidad Católica de Chile, Facultad de Historia, Geografía y Ciencias Políticas, Instituto de Geografía https://ojs.uc.cl/index.php/RGNG/article/view/42865/34695 https://ojs.uc.cl/index.php/RGNG/article/view/42865 Revista de Geografía Norte Grande; Núm. 30 (2003); 7-22 0718-3402 0379-8682 Glaciares de escombros permafrost periglacial Rubble’s glaciers info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículo revisado por pares 2021 ftpunivcchileojs 2023-04-16T12:26:04Z The rock glaciers of the Andes of Santiago de Chile are unsuspicious, but important water resources and play a key role within the debris transport system of this semiarid high mountain area. The significance of these bodies of debris and ice within the geomorphologic and hydrologic system is shown in the case of the Casa de Piedra valley. This subcatchment of the Yeso river is situated very close to the El Yeso reservoir, which is of outstanding importance for the drinking water supply to Santiago. In the Casa de Piedra valley, recent sporadic permafrost in the form of active rock glaciers reaches down to 3000 m a.s.l. Between 3500 and 3800 m a.s.l., active rock glaciers occupy even 16% of the total debris-covered area and represent the predominant landform. Therefore discontinuous mountain permafrost has to be assumed above 3500 m a.s.l. In the study area, debris rock glaciers are observed as well as morrainic rock glaciers, the latter in lower altitudes in the neighborhood of dead ice bodies and the corresponding end morraines. The transition to the nival zone takes place around 3800 m a.s.l. at the recent equilibrium line of glaciers. In the Casa de Piedra valley, more frozen water is stored in active rock glaciers than in “true” glaciers. This situation may be assumed to be representative of many of the small catchments in the Andes of Santiago with elevations below approx. 5000 m a.s.l. Los glaciares de escombros (glaciares de roca, glaciares rocosos) de la Cordillera de Santiago constituyen un insospechado, pero importante recurso hídrico y juegan un papel clave en el sistema de transporte de sedimento de la alta montaña semiárida. Se señala la importancia de estos cuerpos de detrito y hielo en los sistemas geomorfológico e hidrológico tomando el Cajón de la Casa de Piedra como ejemplo. Esta subcuenca del río Yeso se ubica cerca del embalse El Yeso, que es de gran importancia para el abastecimiento de agua para Santiago. El permafrost insular del Cajón de la Casa de Piedra empieza a los 3000 m.s.n.m. en ... Article in Journal/Newspaper Ice permafrost Unknown Alta Hielo ENVELOPE(-58.133,-58.133,-62.083,-62.083) Roca ENVELOPE(-44.817,-44.817,-60.733,-60.733) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftpunivcchileojs |
language |
Spanish |
topic |
Glaciares de escombros permafrost periglacial Rubble’s glaciers |
spellingShingle |
Glaciares de escombros permafrost periglacial Rubble’s glaciers BRENNING, ALEXANDER The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results |
topic_facet |
Glaciares de escombros permafrost periglacial Rubble’s glaciers |
description |
The rock glaciers of the Andes of Santiago de Chile are unsuspicious, but important water resources and play a key role within the debris transport system of this semiarid high mountain area. The significance of these bodies of debris and ice within the geomorphologic and hydrologic system is shown in the case of the Casa de Piedra valley. This subcatchment of the Yeso river is situated very close to the El Yeso reservoir, which is of outstanding importance for the drinking water supply to Santiago. In the Casa de Piedra valley, recent sporadic permafrost in the form of active rock glaciers reaches down to 3000 m a.s.l. Between 3500 and 3800 m a.s.l., active rock glaciers occupy even 16% of the total debris-covered area and represent the predominant landform. Therefore discontinuous mountain permafrost has to be assumed above 3500 m a.s.l. In the study area, debris rock glaciers are observed as well as morrainic rock glaciers, the latter in lower altitudes in the neighborhood of dead ice bodies and the corresponding end morraines. The transition to the nival zone takes place around 3800 m a.s.l. at the recent equilibrium line of glaciers. In the Casa de Piedra valley, more frozen water is stored in active rock glaciers than in “true” glaciers. This situation may be assumed to be representative of many of the small catchments in the Andes of Santiago with elevations below approx. 5000 m a.s.l. Los glaciares de escombros (glaciares de roca, glaciares rocosos) de la Cordillera de Santiago constituyen un insospechado, pero importante recurso hídrico y juegan un papel clave en el sistema de transporte de sedimento de la alta montaña semiárida. Se señala la importancia de estos cuerpos de detrito y hielo en los sistemas geomorfológico e hidrológico tomando el Cajón de la Casa de Piedra como ejemplo. Esta subcuenca del río Yeso se ubica cerca del embalse El Yeso, que es de gran importancia para el abastecimiento de agua para Santiago. El permafrost insular del Cajón de la Casa de Piedra empieza a los 3000 m.s.n.m. en ... |
format |
Article in Journal/Newspaper |
author |
BRENNING, ALEXANDER |
author_facet |
BRENNING, ALEXANDER |
author_sort |
BRENNING, ALEXANDER |
title |
The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results |
title_short |
The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results |
title_full |
The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results |
title_fullStr |
The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results |
title_full_unstemmed |
The Importance of Debris Glaciers in Debris Glaciers in the Geomorphological and Hydrological Systems of the Santiago Mountain Range: Fundamentals and First Results |
title_sort |
importance of debris glaciers in debris glaciers in the geomorphological and hydrological systems of the santiago mountain range: fundamentals and first results |
publisher |
Pontificia Universidad Católica de Chile, Facultad de Historia, Geografía y Ciencias Políticas, Instituto de Geografía |
publishDate |
2021 |
url |
https://ojs.uc.cl/index.php/RGNG/article/view/42865 |
long_lat |
ENVELOPE(-58.133,-58.133,-62.083,-62.083) ENVELOPE(-44.817,-44.817,-60.733,-60.733) |
geographic |
Alta Hielo Roca |
geographic_facet |
Alta Hielo Roca |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
Revista de Geografía Norte Grande; Núm. 30 (2003); 7-22 0718-3402 0379-8682 |
op_relation |
https://ojs.uc.cl/index.php/RGNG/article/view/42865/34695 https://ojs.uc.cl/index.php/RGNG/article/view/42865 |
_version_ |
1767961288867053568 |