Interpretación geomorfológica de las inestabilidades de ladera en el Macizo de Anaga (Tenerife, Islas Canarias)

  1. J. Yepes 1
  2. M.J. Rodríguez-Peces 2
  3. J. Pérez Lentini 3
  1. 1 Universidad de Las Palmas de Gran Canaria
    info

    Universidad de Las Palmas de Gran Canaria

    Las Palmas de Gran Canaria, España

    ROR https://ror.org/01teme464

  2. 2 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  3. 3 Universidad Politécnica de Madrid
    info

    Universidad Politécnica de Madrid

    Madrid, España

    ROR https://ror.org/03n6nwv02

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Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Any de publicació: 2012

Títol de l'exemplar: VIII Congreso Geológico de España, Oviedo, 17-19 de julio, 2012.

Número: 13

Pàgines: 687-690

Tipus: Article

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Altres publicacions en: Geotemas (Madrid)

Resum

This study presents a geomorphologic review of the northern sector of the Anaga Massif in order to establish a relative sequence of geomorphic processes. The present-day relief shows a polygenic nature, combining fluvial erosion with other prior erosive processes. The analysis of slopes and watersheds suggests the existence of an active instability process during the Quaternary. However, the anomalies of the drainage system are related with the differential resistance which shows basic dykes against erosion. Some geomorphologic features suggest the occurrence of an old flank collapse affecting the slopes of Taganana village. This instability will be a stage of the retreatment of the slopes which occurs in a volcanic island along time, in both emerged and submerged flanks.

Fuente de los datos: Dialnet