Evolución geomorfológica de las Lagunas de Ruidera (Albacete-Ciudad Real)
DOI:
https://doi.org/10.3989/egeol.87433-4592Keywords:
Geomorphology, Ruidera pools, fluvio-lacustrine system, Quaternary, fluvial carbonates, calacareous tufs, travertine, travertine dam, travertine pools, water carbonatesAbstract
The Ruidera Pools may be adscribed to fluvio-Iacustrine travertine dams system associated with springs related with karstified jurasic materials. Geomorphological elements of travertine deposits, as dam travertines, terrace travertines, muddy detrital travertine deposits, are described. Older coluvial deposits and present-day valley slope deposits are described also. A geomorphological evolution of Ruidera Pools system supported by both geomorphological elements is proposed.
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Published
1987-08-30
How to Cite
González Martín, J. A., Ordóñez, S., & García del Cura, M. A. (1987). Evolución geomorfológica de las Lagunas de Ruidera (Albacete-Ciudad Real). Estudios Geológicos, 43(3-4), 227–239. https://doi.org/10.3989/egeol.87433-4592
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