Use this link to cite:
http://hdl.handle.net/2183/5976 Síntesis de procesos geomorfológicos en el límite galaico-astur
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Asensio Amor, I.
González Martín, J. A.
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Cadernos do Laboratorio Xeolóxico de Laxe, 1987, 11: 103-111 ISSN: 0213-4497
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Abstract
[Resumen] En este trabajo se analizan los distintos procesos geomorfológicos que han intervenido en el modelado de formas en el sector Galaico-Astur. Actualmente, los procesos de índole dinámica (fluviales, marinos, etc.) y los edafogenéticos son los que muestran una mayor incidencia aunque condicionados por la influencia de factores estructurales y de orden climático; buena parte de su eficacia está favorecida, igualmente, por las acciones antrópicas. En lo que respecta a los procesos antiguos, éstos vuelven a revestir su mayor importancia dentro de la tipología dinámica; no obstante, ellos presentan una originalidad más contrastada al haber actuado bajo condiciones climáticas más rigurosas y extremas, y con niveles de base marinos muy diferentes.
[Abstract] In this synthesis we analyse the several geomorphological processes that have contributed to model the landforms in the «Galaico-Astur» area. At present, the dynamic nature processes (fluvial, marine, etc.) show a greater incidence though they are conditioned by the inf1uén:~ of climatic and structural factors; most of their efficacy results also increased by antrhopactions. As regards the ancient processes, those of dynamic type are again the more important ones. Furthermore, they appear more stressed because their action was performed on different sea-marine levels and their effects were reinforced by extreme and severe climatic conditions.
[Abstract] In this synthesis we analyse the several geomorphological processes that have contributed to model the landforms in the «Galaico-Astur» area. At present, the dynamic nature processes (fluvial, marine, etc.) show a greater incidence though they are conditioned by the inf1uén:~ of climatic and structural factors; most of their efficacy results also increased by antrhopactions. As regards the ancient processes, those of dynamic type are again the more important ones. Furthermore, they appear more stressed because their action was performed on different sea-marine levels and their effects were reinforced by extreme and severe climatic conditions.

