Evolución geomorfológica de las Lagunas de Ruidera (Albacete-Ciudad Real)

J. A. González Martín; S. Ordóñez; Mª A. García del Cura

doi:10.3989/egeol.87433-4592

Evolución geomorfológica de las Lagunas de Ruidera (Albacete-Ciudad Real)

Authors

J. A. González Martín Departamento de Geografía. U.A.M.
S. Ordóñez Departamento de Petrología. U.C.M.
Mª A. García del Cura Instituto de Geología Económica. C.S.I.C.-U.C.M.

DOI:

https://doi.org/10.3989/egeol.87433-4592

Keywords:

Geomorphology, Ruidera pools, fluvio-lacustrine system, Quaternary, fluvial carbonates, calacareous tufs, travertine, travertine dam, travertine pools, water carbonates

Abstract

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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Issue

Vol. 43 No. 3-4 (1987)

Section

Articles

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