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handle: 10261/23300
Las Lagunas de Ruidera pueden considerarse un sistema fluvio-Iacustre de represas travertínicas asociadas a exurgencia kársticas. Se describen los elementos geomorfológicos de estos depósitos travertínicos: edificios de barrera, terrazas travertínicas, depósitos carbonáticos detríticos, así como los elementos geomorfológicos detríticos existentes: acumulaciones de ladera, de fondo de valle, etc. A partir de ambos se establece un esquema de evolución geomorfológica del sistema fluviolacustre de Ruidera.
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Represas travertínicas, Travertine pools, cuaternario, travertinos, carbonatos fluviales, Ruidera pools, Travertinos, Tobas calcáreas, Travertine dam, fluvio-lacustrine system, water carbonates, fluvial carbonates, Quaternary, lagunas travertínicas, sistema fluvio-lacustre, travertine, calacareous tufs, tobas calcáreas, Cuaternario, Lagunas travertínicas, Travertine, QE1-996.5, travertine pools, Lagunas de Ruidera, travertine dam, lagunas de ruidera, Geology, represas travertínicas, Geomorphology, carbonatos de cascada, Carbonatos de cascada, Geomorfología, Calacareous tufs, Water carbonates, Fluvial carbonates, Carbonatos fluviales, Sistema fluvio-lacustre, geomorfología, Fluvio-lacustrine system
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