Morphogenesis of karst poljes on Vis Island, Croatia

[EN] Karst poljes are the most characteristic feature of Dinaric karst area. The number of poljes identified on the island of Vis (Croatia) differs according to the various authors who have studied the island. Considering the various existing definitions of polje in previous studies, in this paper w...

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Detalles Bibliográficos
Autores: Krklec, Kristina, Lozic, Sanja, Siljeg, Ante, Perica, Drazen, Siljeg, Silvija
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:España
Institución:Universidad de Salamanca (USAL)
Repositorio:GREDOS. Repositorio Institucional de la Universidad de Salamanca
OAI Identifier:oai:gredos.usal.es:10366/163217
Acceso en línea:http://hdl.handle.net/10366/163217
Access Level:acceso abierto
Palabra clave:karst polje
Morphogenesis
Vis island
2506 Geología
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spelling Morphogenesis of karst poljes on Vis Island, CroatiaKrklec, KristinaLozic, SanjaSiljeg, AntePerica, DrazenSiljeg, Silvijakarst poljeMorphogenesisVis island2506 Geología[EN] Karst poljes are the most characteristic feature of Dinaric karst area. The number of poljes identified on the island of Vis (Croatia) differs according to the various authors who have studied the island. Considering the various existing definitions of polje in previous studies, in this paper we propose a set of criteria for identifying poljes in karst terrain using Geographic Information System. This enabled the identification of six poljes on the Vis Island, whose formation is predetermined by tectonic structures. Moreover, processes are frequently inferred by neotectonic (both uplift and subsidence) according to the analysis of longitudinal and transverse profiles gradients affecting balance of these morphologies. Since they are not hydrologically active in present hydrological conditions, poljes on Vis Island can be considered to be paleo - overflow or structural poljes.202520252015info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/10366/163217reponame:GREDOS. Repositorio Institucional de la Universidad de Salamancainstname:Universidad de Salamanca (USAL)InglésAttribution-NonCommercial-NoDerivatives 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessoai:gredos.usal.es:10366/1632172026-06-07T06:28:51Z
dc.title.none.fl_str_mv Morphogenesis of karst poljes on Vis Island, Croatia
title Morphogenesis of karst poljes on Vis Island, Croatia
spellingShingle Morphogenesis of karst poljes on Vis Island, Croatia
Krklec, Kristina
karst polje
Morphogenesis
Vis island
2506 Geología
title_short Morphogenesis of karst poljes on Vis Island, Croatia
title_full Morphogenesis of karst poljes on Vis Island, Croatia
title_fullStr Morphogenesis of karst poljes on Vis Island, Croatia
title_full_unstemmed Morphogenesis of karst poljes on Vis Island, Croatia
title_sort Morphogenesis of karst poljes on Vis Island, Croatia
dc.creator.none.fl_str_mv Krklec, Kristina
Lozic, Sanja
Siljeg, Ante
Perica, Drazen
Siljeg, Silvija
author Krklec, Kristina
author_facet Krklec, Kristina
Lozic, Sanja
Siljeg, Ante
Perica, Drazen
Siljeg, Silvija
author_role author
author2 Lozic, Sanja
Siljeg, Ante
Perica, Drazen
Siljeg, Silvija
author2_role author
author
author
author
dc.subject.none.fl_str_mv karst polje
Morphogenesis
Vis island
2506 Geología
topic karst polje
Morphogenesis
Vis island
2506 Geología
description [EN] Karst poljes are the most characteristic feature of Dinaric karst area. The number of poljes identified on the island of Vis (Croatia) differs according to the various authors who have studied the island. Considering the various existing definitions of polje in previous studies, in this paper we propose a set of criteria for identifying poljes in karst terrain using Geographic Information System. This enabled the identification of six poljes on the Vis Island, whose formation is predetermined by tectonic structures. Moreover, processes are frequently inferred by neotectonic (both uplift and subsidence) according to the analysis of longitudinal and transverse profiles gradients affecting balance of these morphologies. Since they are not hydrologically active in present hydrological conditions, poljes on Vis Island can be considered to be paleo - overflow or structural poljes.
publishDate 2015
dc.date.none.fl_str_mv 2015
2025
2025
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10366/163217
url http://hdl.handle.net/10366/163217
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.rights.none.fl_str_mv Attribution-NonCommercial-NoDerivatives 4.0 Internacional
http://creativecommons.org/licenses/by-nc-nd/4.0/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Attribution-NonCommercial-NoDerivatives 4.0 Internacional
http://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv reponame:GREDOS. Repositorio Institucional de la Universidad de Salamanca
instname:Universidad de Salamanca (USAL)
instname_str Universidad de Salamanca (USAL)
reponame_str GREDOS. Repositorio Institucional de la Universidad de Salamanca
collection GREDOS. Repositorio Institucional de la Universidad de Salamanca
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,811543

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