Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain)
Signs of hypogenic speleogenesis have been detected in a number of caves of the Murcia Region (SE Spain), in some cases revealing active speleogenetic mechanisms rarely observed in hypogene cavities elsewhere in the world. Here, we investigate the hypogenic morphologies and speleothems of four caves...
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ftusouthflorida:oai:digitalcommons.usf.edu:kip_articles-7517 2023-12-03T10:21:01+01:00 Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) Gázquez, Fernando Calaforra, José María Rodríguez-Estrella, Tomás 2017-08-17T07:00:00Z https://digitalcommons.usf.edu/kip_articles/6517 https://doi.org/10.1007/978-3-319-53348-3_4 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/kip_articles/6517 doi:10.1007/978-3-319-53348-3_4 https://doi.org/10.1007/978-3-319-53348-3_4 KIP Articles Hypogenic caves Hydrothermal speleogenesis Hydrothermal speleothems text 2017 ftusouthflorida https://doi.org/10.1007/978-3-319-53348-3_4 2023-11-05T17:28:01Z Signs of hypogenic speleogenesis have been detected in a number of caves of the Murcia Region (SE Spain), in some cases revealing active speleogenetic mechanisms rarely observed in hypogene cavities elsewhere in the world. Here, we investigate the hypogenic morphologies and speleothems of four caves in this region, namely Sima de la Higuera, Sima Destapada, Cueva del Agua and Cueva del Puerto. Also, other ten caves showing evidence for hypogenic speleogenesis has been preliminary described. Processes related to ancient and current hydrothermal activity, the discordance of permeability structures in the adjacent beds and the spatial arrangement of the regional hydrogeology have given rise to maze patterns and typical subaqueous hypogenic morphologies. These include spongework mazes, rising wall channels and shafts, feeders, bubble trails, solution pockets, megascallops and rising of chains cupolas, among others. Carbonic acid speleogenesis is responsible for the formation of most of these cave features; however, evidence of sulfuric acid speleogenesis (SAS) has been observed in Cueva del Puerto and Sima del Pulpo, which host massive secondary gypsum deposits. Speleothems typically linked to hydrothermal water upwelling and CO2 degassing close to the water table are present in most of these cavities, including folia, calcite spar crystals, cave clouds, calcite rafts deposits and several types of cave raft cones. The wide variety of hypogenic speleogenesis indicators and speleothems whose genesis is unconnected to meteoric water seepage reveals that the hydrothermal field of the Murcia Region hosts one of the densest active hypogenic subterranean networks in the world. Text Carbonic acid University of South Florida St. Petersburg: Digital USFSP Cueva ENVELOPE(-62.600,-62.600,-64.150,-64.150) Cones The ENVELOPE(78.344,78.344,-68.635,-68.635) Cones, The ENVELOPE(78.344,78.344,-68.635,-68.635) 85 97 |
institution |
Open Polar |
collection |
University of South Florida St. Petersburg: Digital USFSP |
op_collection_id |
ftusouthflorida |
language |
unknown |
topic |
Hypogenic caves Hydrothermal speleogenesis Hydrothermal speleothems |
spellingShingle |
Hypogenic caves Hydrothermal speleogenesis Hydrothermal speleothems Gázquez, Fernando Calaforra, José María Rodríguez-Estrella, Tomás Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) |
topic_facet |
Hypogenic caves Hydrothermal speleogenesis Hydrothermal speleothems |
description |
Signs of hypogenic speleogenesis have been detected in a number of caves of the Murcia Region (SE Spain), in some cases revealing active speleogenetic mechanisms rarely observed in hypogene cavities elsewhere in the world. Here, we investigate the hypogenic morphologies and speleothems of four caves in this region, namely Sima de la Higuera, Sima Destapada, Cueva del Agua and Cueva del Puerto. Also, other ten caves showing evidence for hypogenic speleogenesis has been preliminary described. Processes related to ancient and current hydrothermal activity, the discordance of permeability structures in the adjacent beds and the spatial arrangement of the regional hydrogeology have given rise to maze patterns and typical subaqueous hypogenic morphologies. These include spongework mazes, rising wall channels and shafts, feeders, bubble trails, solution pockets, megascallops and rising of chains cupolas, among others. Carbonic acid speleogenesis is responsible for the formation of most of these cave features; however, evidence of sulfuric acid speleogenesis (SAS) has been observed in Cueva del Puerto and Sima del Pulpo, which host massive secondary gypsum deposits. Speleothems typically linked to hydrothermal water upwelling and CO2 degassing close to the water table are present in most of these cavities, including folia, calcite spar crystals, cave clouds, calcite rafts deposits and several types of cave raft cones. The wide variety of hypogenic speleogenesis indicators and speleothems whose genesis is unconnected to meteoric water seepage reveals that the hydrothermal field of the Murcia Region hosts one of the densest active hypogenic subterranean networks in the world. |
format |
Text |
author |
Gázquez, Fernando Calaforra, José María Rodríguez-Estrella, Tomás |
author_facet |
Gázquez, Fernando Calaforra, José María Rodríguez-Estrella, Tomás |
author_sort |
Gázquez, Fernando |
title |
Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) |
title_short |
Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) |
title_full |
Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) |
title_fullStr |
Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) |
title_full_unstemmed |
Evidence for Regional Hypogene Speleogenesis in Murcia (SE Spain) |
title_sort |
evidence for regional hypogene speleogenesis in murcia (se spain) |
publisher |
Digital Commons @ University of South Florida |
publishDate |
2017 |
url |
https://digitalcommons.usf.edu/kip_articles/6517 https://doi.org/10.1007/978-3-319-53348-3_4 |
long_lat |
ENVELOPE(-62.600,-62.600,-64.150,-64.150) ENVELOPE(78.344,78.344,-68.635,-68.635) ENVELOPE(78.344,78.344,-68.635,-68.635) |
geographic |
Cueva Cones The Cones, The |
geographic_facet |
Cueva Cones The Cones, The |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
KIP Articles |
op_relation |
https://digitalcommons.usf.edu/kip_articles/6517 doi:10.1007/978-3-319-53348-3_4 https://doi.org/10.1007/978-3-319-53348-3_4 |
op_doi |
https://doi.org/10.1007/978-3-319-53348-3_4 |
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