El hidrolacolito de las Calderuelas (Parque Nacional de la Sierra de Guadarrama), una morfología periglaciar singular

[EN] This research describes the finding of a hydro-laccolith in the Sierra de Guadarrama (Central System). The study, based on the combination of Digital Terrain Models (DTM) and geoelectric data, allowed the characterization of the surface morphology and inter- nal structure. The results allow est...

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Detalles Bibliográficos
Autores: Carrasco, Rosa M., Pedraza, Javier, Férnandez Lozano, Javier, Sánchez Vizcaíno, Jesús, L. Soteres, Rodrigo, Karampaglidis, Theodoros, Turu, Valentí, Ros, Xavier, Merlo, Oscar
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2020
País:España
Institución:Universidad de León
Repositorio:BULERIA. Repositorio Institucional de la Universidad de León
OAI Identifier:oai:buleria.unileon.es:10612/21613
Acceso en línea:https://hdl.handle.net/10612/21613
Access Level:acceso abierto
Palabra clave:Ingeniería de minas
Hidrolacolito
Periglaciar
Lidar
Geoeléctrico
Par- Que Nacional Sierra De Guadarrama (españa).
Descripción
Sumario:[EN] This research describes the finding of a hydro-laccolith in the Sierra de Guadarrama (Central System). The study, based on the combination of Digital Terrain Models (DTM) and geoelectric data, allowed the characterization of the surface morphology and inter- nal structure. The results allow establishing the genesis of this pe- riglacial-related structure and the role played by slope processes in its evolution. Freeze-thawing cycles and hydrogeological conditions are responsible factors that control its evolution over time. Such type of structures show an extraordinary environmental sensitivity, thus their monitoring is of great interest to guarantee their further pre- servation.

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