Mechanisms associated with the erosion of sand dune cliffs, Magilligan, Northern Ireland
Auteurs :CARTER, R. W. G.
STONE, G. W.
Description :
A fifteen year history of coastal dune recession at Magillan, has revealed both time and space contrasts in processes and morphology. Since 1968 storm frequency has increased, while dune retreat reached a peak in 1978-1979. Three types of dune eroding events are noted, resulting from particular wave, wind, tide combinations. The spatial variability in dune scarping is associated with vegetation and soil development, and slope failures range from granular avalanches to retrogressive rotational slumps.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 1989, vol. 14, n°. 1, p. 1-10, Références bibliographiques : 17 réf.
Date :
1989
Editeur :
Pays édition : Royaume-Uni, Chichester, Wiley
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)