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Groundwater flow in a relatively old oceanic volcanic island: the Betancuria area, Fuerteventura Island, Canary Islands, Spain

Autor
Herrera Lameli, Ch.; Custodio, E.
Tipus d'activitat
Article en revista
Revista
Science of the total environment
Data de publicació
2014-10-15
Volum
496
Pàgina inicial
531
Pàgina final
550
DOI
https://doi.org/10.1016/j.scitotenv.2014.07.063 Obrir en finestra nova
Projecte finançador
PROCESOS DE RECARGA Y DESCARGA DE ACUIFEROS MEDIANTE TRAZADORES NATURALES: APLICACION AL AREA MEDITERRANEA
Palaeaux management of coastal aquifers in europe : palaeowaters, natural controls and human influence
URL
http://www.sciencedirect.com/science/article/pii/S0048969714010936 Obrir en finestra nova
Resum
The island of Fuerteventura is the oldest of the Canary Islands' volcanic archipelago. It is constituted by volcanic submarine and subaerial activity and intrusive Miocene events, with some residual later volcanism and Quaternary volcanic deposits that have favored groundwater recharge. The climate is arid, with an average rainfall that barely attains 60mm/year in the coast and up to 200mm/year in the highlands. The aquifer recharge is small but significant; it is brackish due to large airborne ...
Paraules clau
Canary Islands, Conceptual hydrogeological model, Fuerteventura Island, Groundwater recharge, Old volcanic island, Spain
Grup de recerca
GHS - Grup d'Hidrologia Subterrània

Participants