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Par Collection Par Auteur- PSUTY, N. (3)
- ZAZO, C. (3)
- PACE, J.P. (1)
- ROBERTS, H.M. (1)
- STUPPLES, P. (1)
- TOLGENSBAKK, J. (1)
- PLATER, A.J. (1)
- PSUTY, N.P. (1)
- SANJAUME, E. (1)
- 2009 (3)
- Aménagement du littoral ; Bilan sédimentaire ; Dynamique littorale ; Erosion littorale ; Etats-Unis ; Géomorphologie littorale ; Littoral ; Lutte contre l'érosion ; New Jersey ; Politique locale (1)
- Balance sedimentario ; Dinámica litoral ; Erosión litoral ; Geomorfología litoral ; Litoral ; Lucha contra la erosión ; Ordenamientodel litoral ; Política local (1)
- Barrier effect ; England ; Grain size distribution ; Holocene ; Intertidal zone ; Kent ; Marine quaternary ; Marine sedimentation ; Sea level ; Tidal marsh ; United Kingdom (1)
- Beach ridge ; Climatic variation ; Coastal dynamics ; Coastal environment ; Coastal geomorphology ; Cold area ; Glacial features ; Norway ; Norwegian Sea ; Sediment transport ; Vertical movement (1)
- Coastal dynamics ; Coastal environment ; Coastal erosion ; Coastal geomorphology ; Coastal management ; Erosion control ; Local policy ; New Jersey ; Sediment budget ; United States of America (1)
- Cuaternario marino ; Efecto de relieve ; Granulometría ; Holoceno ; Marisma litoral ; Nivel del mar ; Sedimentación marina ; Zona intertidal (1)
- Dinámica litoral ; Geomorfología litoral ; Glaciar ; Litoral ; Movimiento vertical ; Transporte sedimentario ; Variación climática ; Zona fría (1)
- Dynamique littorale ; Glaciaire ; Géomorphologie littorale ; Levée de plage ; Littoral ; Mer de Norvège ; Mouvement vertical ; Norvège ; Transport sédimentaire ; Variation climatique ; Zone froide (1)
Beach ridges from the Varanger Peninsula (Arctic Norwegian coast) : characteristics and significance
- evolution (sediment supply, offshore gradient and coastal evolution). These differences between various or parts of the same bay invalidate the explanations that global processes (planetary orbital forces, relative sea-level changes or past climatic
- , the inter-relationship and inter-dependence between gravel barrier and marshland environments, and, ultimately, the significance of relative sea-level rise, coastal morphology, storm events, and sediment supply in shaping the Dungeness and Romney Marsh
- , and subsequently at Gunnison Beach, a site of sediment accumulation. A new management philosophy of smaller scale restoration of sediment supply in the Critical Zone has emerged.