Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain)
El Salt is an episodic waterfall located in the city of Alcoy (Spain), Alicante. The Barxell River Source, has calcium bicarbonate waters and an estimated flow rate of 17,000 m3 / day. It is a potential tufa generator, with an estimated generation capacity of up to 1,240 t / year. The tufa deposits...
| Autores: | , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2016 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | inglés |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13552 |
| Acceso en línea: | http://hdl.handle.net/10272/13552 |
| Access Level: | acceso abierto |
| Palabra clave: | Fluvial tufa Pleistocene Carbonate build-ups Seep tufa Waterfall Toba fluvial Edificios carbonáticos Toba de rezume Cascada |
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Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain)Arquitectura de sistemas fluviales tobáceos pleistocenos asociados con cascadas: El Salt (Alcoy, España)Ordóñez, SalvadorCuevas González, JaimeBenavente, DavidGarcía del Cura, María AngelesFluvial tufaPleistoceneCarbonate build-upsSeep tufaWaterfallToba fluvialEdificios carbonáticosToba de rezumeCascadaEl Salt is an episodic waterfall located in the city of Alcoy (Spain), Alicante. The Barxell River Source, has calcium bicarbonate waters and an estimated flow rate of 17,000 m3 / day. It is a potential tufa generator, with an estimated generation capacity of up to 1,240 t / year. The tufa deposits located along Barxell River relates to the geomorphologic evolution of valley. Upstream the active waterfall it found a tufa river terrace T (+20 m). Downstream cascade, several types of tufa deposits links to two stages of geomorphologic evolution of the valley: a) The distal progradation tufa deposits related to a “non-effective to base-level change incision”, described as piedmont or progradation tufa build-ups T-1, T-2 and T-3; and b) The post "incisional base level change" tufa deposits, Font del Quinzet (T-4) tufa barrier, associated with back-lake sediments, and finally active tufa seeps on cliff (T-5)Sociedad Geológica de España20162016-01-0120162016-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/13552reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/135522026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) Arquitectura de sistemas fluviales tobáceos pleistocenos asociados con cascadas: El Salt (Alcoy, España) |
| title |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) |
| spellingShingle |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) Ordóñez, Salvador Fluvial tufa Pleistocene Carbonate build-ups Seep tufa Waterfall Toba fluvial Edificios carbonáticos Toba de rezume Cascada |
| title_short |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) |
| title_full |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) |
| title_fullStr |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) |
| title_full_unstemmed |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) |
| title_sort |
Architecture of Pleistocene fluvial tufa systems associated with waterfalls: El Salt (Alcoy, Spain) |
| dc.creator.none.fl_str_mv |
Ordóñez, Salvador Cuevas González, Jaime Benavente, David García del Cura, María Angeles |
| author |
Ordóñez, Salvador |
| author_facet |
Ordóñez, Salvador Cuevas González, Jaime Benavente, David García del Cura, María Angeles |
| author_role |
author |
| author2 |
Cuevas González, Jaime Benavente, David García del Cura, María Angeles |
| author2_role |
author author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Fluvial tufa Pleistocene Carbonate build-ups Seep tufa Waterfall Toba fluvial Edificios carbonáticos Toba de rezume Cascada |
| topic |
Fluvial tufa Pleistocene Carbonate build-ups Seep tufa Waterfall Toba fluvial Edificios carbonáticos Toba de rezume Cascada |
| description |
El Salt is an episodic waterfall located in the city of Alcoy (Spain), Alicante. The Barxell River Source, has calcium bicarbonate waters and an estimated flow rate of 17,000 m3 / day. It is a potential tufa generator, with an estimated generation capacity of up to 1,240 t / year. The tufa deposits located along Barxell River relates to the geomorphologic evolution of valley. Upstream the active waterfall it found a tufa river terrace T (+20 m). Downstream cascade, several types of tufa deposits links to two stages of geomorphologic evolution of the valley: a) The distal progradation tufa deposits related to a “non-effective to base-level change incision”, described as piedmont or progradation tufa build-ups T-1, T-2 and T-3; and b) The post "incisional base level change" tufa deposits, Font del Quinzet (T-4) tufa barrier, associated with back-lake sediments, and finally active tufa seeps on cliff (T-5) |
| publishDate |
2016 |
| dc.date.none.fl_str_mv |
2016 2016-01-01 2016 2016-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10272/13552 |
| url |
http://hdl.handle.net/10272/13552 |
| 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 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Sociedad Geológica de España |
| publisher.none.fl_str_mv |
Sociedad Geológica de España |
| dc.source.none.fl_str_mv |
reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva instname:Universidad de Huelva (UHU) |
| instname_str |
Universidad de Huelva (UHU) |
| reponame_str |
Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| collection |
Arias Montano. Repositorio Institucional de la Universidad de Huelva |
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15.812455 |