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A l’embouchure de l’Assif Tamraght, une basse terrasse côtière se développe entre le pied d’une falaise morte situé autour de +8 m et l’Océan. Cette terrasse recèle le témoignage des fluctuations du niveau de la mer qui se sont produites pendant le MIS 5
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Géomorphologie relief processus environnement, 2000
Abstract Along the 50 km of coastline from Villa San Giovanni to Mèlito di Porto Salvo, fourteen marine terraces (so-called main terraces) form a staircase between the present sea-level and 520 m a. s. I. They were uplifted at a mean rate of 1.24m/ka. Their minimum width is 60 m and their are often bounded landward by a former sea-cliff more than 10 m ...
Dumas, Bernard +3 more
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Abstract Along the 50 km of coastline from Villa San Giovanni to Mèlito di Porto Salvo, fourteen marine terraces (so-called main terraces) form a staircase between the present sea-level and 520 m a. s. I. They were uplifted at a mean rate of 1.24m/ka. Their minimum width is 60 m and their are often bounded landward by a former sea-cliff more than 10 m ...
Dumas, Bernard +3 more
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Succession et âges radiométriques des terrasses marines du levant espagnol
Bulletin de l'Association française pour l'étude du quaternaire, 1977Dumas Bernard. Succession et âges radiométriques des terrasses marines du levant espagnol. In: Bulletin de l'Association française pour l'étude du quaternaire, vol. 14, n°4, 1977. pp. 82-85.
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Sols polygonaux et « terrasses marines » au Spitzberg
Revue de géographie de Lyon, 1954Corbel Jean. Sols polygonaux et « terrasses marines » au Spitzberg. In: Revue de géographie de Lyon, vol. 29, n°1, 1954. pp. 1-28.
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Néotectonique, terrasses et niveaux marins de la plaine du Sélé (Italie du Sud)
Bulletin de l'Association française pour l'étude du quaternaire, 1975Lo studio morfologico e sedimentologico delle terrazze della Pianura litorale del Sele (Italia Meridionale) permette di distinguervi tre falde alluvionali. I seguiti di minerali pesanti ch'esse contengono ed i loro rapporti con le paleo-rive mettono in evidenza che le due più basse sono tardive e d'origine eustatica (interstadio Würm II — III, poi post-
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Les Terrasses D'Abrasion Marine de la Cote Libanaise
Geographical Review, 1948H. E. Wright, Etienne de Vaumas
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