IGB

Connexion

(Article of periodic en Anglais - 1985)

Document title

The origin of foredunes and sandy beach ridges

Authors(s) and Affiliation(s)

BIRD E. C. F. ;

Abstract

Studies of prograded sectors of sandy coastline in Victoria have shown that some are initiated upon wave-built beach berms colonised by dune vegetation that begins to trap wind blown sand| others develop where backshore terraces built under dune vegetation spreading from pre-existing dunes are trimmed back by storm wave erosion, forming a dune cliff capped by spillover sand which becomes a foredune as further aeolian accretion proceeds. A berm is defined as an impersistant wave-built ridge or terrace on the beach face| a beach ridge is a more persistent wave-built ridge formed at or above high spring tide on a prograding sandy coast| a foredune is a ridge of aeolian sand running parallel to the coastline. (L'A.).

Source

Article of periodic

published at : Search Sydney

Editor :

Millesime : 1985, vol. 16, no3-4 [pp. 109-111]

Bibliographic references : 8 réf.

Language

Anglais

Refdoc record number (ud4) : 12187916 : Permanent link - XML version
Powered by Pxxo