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

Erakutsi afiliazioak +
Aldizkaria:
Geotemas (Madrid)

ISSN: 1576-5172

Argitalpen urtea: 2012

Zenbakien izenburua: VIII Congreso Geológico de España, Oviedo, 17-19 de julio, 2012.

Zenbakia: 13

Orrialdeak: 687-690

Mota: Artikulua

DIALNET GOOGLE SCHOLAR

Beste argitalpen batzuk: Geotemas (Madrid)

Laburpena

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.

Datuen iturria: Dialnet