La «Fana» de Genestazaun ejemplo de sistema torrencial activo en la Cordillera Cantábrica

  1. Montserrat Jiménez Sánchez 1
  2. Rosana Menéndez Duarte 1
  3. Pedro Farias Arquer 1
  4. Susana Fernández Menéndez 1
  1. 1 Universidad de Oviedo
    info

    Universidad de Oviedo

    Oviedo, España

    ROR https://ror.org/006gksa02

Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1996

Número: 20

Páginas: 1109-1111

Tipo: Artículo

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Otras publicaciones en: Geogaceta

Resumen

«La Fana de Genestaza» is an active mountain torrent representative of these kind of systems in the Cantabrian Moµntains. As the field evir:lences show, the availability of non consolidated material in the catchment area is due to rockfall processes as well as to small landslides. Although water transport processes are prevailing, sporadic discharges of debris-flow take place in the drainage channel. This process is controlled not only by the rainfall regime but also by the volume of available material in the catchment area. The field evidences suggest a relatively high frequency far the occurrence of this kind of episodes.

Fuente de los datos: Dialnet