Publication: Los volcanes de barro o «salsas» : fenómenos hidrogeológicos de
interés ecológico
Authors
González-Bernáldez, F. ; Herrera, P. ; Montes, C.
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Facultad de Biología
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Publisher
Murcia: Universidad de Murcia, Servicio de Publicaciones
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DOI
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info:eu-repo/semantics/article
Description
Abstract
Los volcanes de barro, salsas (mound son formaciones
cas que no tienen que ver con fenómenos hidrotermales o volcánicos aunque superficialmente sean semejantes.
Aparecen, junto con otras características paisajísticas, en zonas de descarga regional de aguas subterráneas y
se deben al componente vertical ascendente del agua salina que provoca la dispersión de la arcilla y la
perforación de una capa confinante poco permeable. Son la manifestación más espectacular de un conjunto de
características (salgüeros, ojos, rezumaderos, etc.) ligadas a veces genéticamente y que acompañan a una
fauna y una flora características de los ecosistemas de descarga de acuíferos.
Mud volcanoes, mound spring craters and soapholes are hydrogeological formations that are not related to hydrothermal or volcanic phenomena being structurally similar. They appear in of ter discharge along with other landscape characteristic of such They appear due to the upward vertical movement of saline waters that cause dispersion and the perforation of confining low permeability layers. They are one of the most conspicuous of a group of genetically related landscape efflorescences, seepage etc.) that are accompagnied by flora and fauna characteristic of aquifer discharge ecosystems.
Mud volcanoes, mound spring craters and soapholes are hydrogeological formations that are not related to hydrothermal or volcanic phenomena being structurally similar. They appear in of ter discharge along with other landscape characteristic of such They appear due to the upward vertical movement of saline waters that cause dispersion and the perforation of confining low permeability layers. They are one of the most conspicuous of a group of genetically related landscape efflorescences, seepage etc.) that are accompagnied by flora and fauna characteristic of aquifer discharge ecosystems.
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