Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain)
A detailed geomorphological map of the Campo de Calatrava Volcanic Field (CCVF) is presented at a scale of 1:50,000. The Campo de Calatrava, located on the south-eastern edge of the Hercynian Massif, is one of the most unusual volcanic areas of the Iberian Peninsula. The volcanic activity develops c...
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2016 |
| País: | España |
| Institución: | Universidad de Oviedo (UNIOVI) |
| Repositorio: | RUO. Repositorio Institucional de la Universidad de Oviedo |
| Idioma: | inglés |
| OAI Identifier: | oai:digibuo.uniovi.es:10651/39970 |
| Acceso en línea: | http://hdl.handle.net/10651/39970 https://dx.doi.org/10.1080/17445647.2016.1195302 |
| Access Level: | acceso abierto |
| Palabra clave: | Geomorphology Mapping Volcanism Campo de Calatrava, Ciudad Realolcanism, Campo de Calatrava Ciudad Real |
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Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain)Poblete Piedrabuena, Miguel Ángel|||0000-0003-1030-5310Beato Bergua, Salvador|||0000-0001-5538-7685Marino Alfonso, José Luis|||0000-0001-6213-407XGeomorphologyMappingVolcanismCampo de Calatrava, Ciudad Realolcanism, Campo de CalatravaCiudad RealA detailed geomorphological map of the Campo de Calatrava Volcanic Field (CCVF) is presented at a scale of 1:50,000. The Campo de Calatrava, located on the south-eastern edge of the Hercynian Massif, is one of the most unusual volcanic areas of the Iberian Peninsula. The volcanic activity develops chronologically from Upper Miocene to Holocene, with a wide range of styles and eruptive dynamics that have created a variety of forms and types of volcanoes, the abundance of maars being outstanding. Thus, this map represents both the landforms of volcanic origin and the interferences that volcanic activity has caused in other processes and forms, offering the reader the key to understanding the origin and fundamental features of the landscape of the territory. Also shown is the crucial role geomorphological mapping can play as a basic tool in the conservation of natural heritage and in territorial planning. The mapping system applied is the French CNRS RCP 77, although various local adaptations have been incorporated. The map legend consists of 80 elements arranged in 10 sections, in which a wide variety of morphostructures, forms and deposits produced under varios types of both relict and active morphogenetic systems are identified.Taylor & Francis Open20162016-01-01journal articlehttp://purl.org/coar/resource_type/c_6501NAhttp://purl.org/coar/version/c_be7fb7dd8ff6fe43info:eu-repo/semantics/articlehttp://hdl.handle.net/10651/39970https://dx.doi.org/10.1080/17445647.2016.1195302Scopushttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84974831069&partnerID=40&md5=13c06ed9056a21934d5abd7764587b4areponame:RUO. Repositorio Institucional de la Universidad de Oviedoinstname:Universidad de Oviedo (UNIOVI)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Attribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessoai:digibuo.uniovi.es:10651/399702026-06-07T06:38:51Z |
| dc.title.none.fl_str_mv |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| title |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| spellingShingle |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) Poblete Piedrabuena, Miguel Ángel|||0000-0003-1030-5310 Geomorphology Mapping Volcanism Campo de Calatrava, Ciudad Realolcanism, Campo de Calatrava Ciudad Real |
| title_short |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| title_full |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| title_fullStr |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| title_full_unstemmed |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| title_sort |
Landforms in the Campo de Calatrava Volcanic Field (Ciudad Real, Central Spain) |
| dc.creator.none.fl_str_mv |
Poblete Piedrabuena, Miguel Ángel|||0000-0003-1030-5310 Beato Bergua, Salvador|||0000-0001-5538-7685 Marino Alfonso, José Luis|||0000-0001-6213-407X |
| author |
Poblete Piedrabuena, Miguel Ángel|||0000-0003-1030-5310 |
| author_facet |
Poblete Piedrabuena, Miguel Ángel|||0000-0003-1030-5310 Beato Bergua, Salvador|||0000-0001-5538-7685 Marino Alfonso, José Luis|||0000-0001-6213-407X |
| author_role |
author |
| author2 |
Beato Bergua, Salvador|||0000-0001-5538-7685 Marino Alfonso, José Luis|||0000-0001-6213-407X |
| author2_role |
author author |
| dc.subject.none.fl_str_mv |
Geomorphology Mapping Volcanism Campo de Calatrava, Ciudad Realolcanism, Campo de Calatrava Ciudad Real |
| topic |
Geomorphology Mapping Volcanism Campo de Calatrava, Ciudad Realolcanism, Campo de Calatrava Ciudad Real |
| description |
A detailed geomorphological map of the Campo de Calatrava Volcanic Field (CCVF) is presented at a scale of 1:50,000. The Campo de Calatrava, located on the south-eastern edge of the Hercynian Massif, is one of the most unusual volcanic areas of the Iberian Peninsula. The volcanic activity develops chronologically from Upper Miocene to Holocene, with a wide range of styles and eruptive dynamics that have created a variety of forms and types of volcanoes, the abundance of maars being outstanding. Thus, this map represents both the landforms of volcanic origin and the interferences that volcanic activity has caused in other processes and forms, offering the reader the key to understanding the origin and fundamental features of the landscape of the territory. Also shown is the crucial role geomorphological mapping can play as a basic tool in the conservation of natural heritage and in territorial planning. The mapping system applied is the French CNRS RCP 77, although various local adaptations have been incorporated. The map legend consists of 80 elements arranged in 10 sections, in which a wide variety of morphostructures, forms and deposits produced under varios types of both relict and active morphogenetic systems are identified. |
| publishDate |
2016 |
| dc.date.none.fl_str_mv |
2016 2016-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 NA http://purl.org/coar/version/c_be7fb7dd8ff6fe43 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10651/39970 https://dx.doi.org/10.1080/17445647.2016.1195302 |
| url |
http://hdl.handle.net/10651/39970 https://dx.doi.org/10.1080/17445647.2016.1195302 |
| dc.language.none.fl_str_mv |
Inglés eng |
| language_invalid_str_mv |
Inglés |
| language |
eng |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
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open access http://purl.org/coar/access_right/c_abf2 Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ |
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openAccess |
| dc.publisher.none.fl_str_mv |
Taylor & Francis Open |
| publisher.none.fl_str_mv |
Taylor & Francis Open |
| dc.source.none.fl_str_mv |
Scopus https://www.scopus.com/inward/record.uri?eid=2-s2.0-84974831069&partnerID=40&md5=13c06ed9056a21934d5abd7764587b4a reponame:RUO. Repositorio Institucional de la Universidad de Oviedo instname:Universidad de Oviedo (UNIOVI) |
| instname_str |
Universidad de Oviedo (UNIOVI) |
| reponame_str |
RUO. Repositorio Institucional de la Universidad de Oviedo |
| collection |
RUO. Repositorio Institucional de la Universidad de Oviedo |
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1869410144492716032 |
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15,300719 |