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Par Collection Par Auteur- FRENCH, H.M. (3)
- KOSTER, E.A. (3)
- AUZET, A.V. (1)
- VAN VLIET-LANOE, B. (1)
- VANDENBERGHE, J. (1)
- COUTARD, J.P. (1)
- HALL, K. (1)
- VAN HUISSTEDEN, J. (1)
- 1988 (3)
- Physical geography (3)
- Creep ; Expérimentation ; Gel ; Granulométrie ; Gélifluxion ; Géographie physique ; Géomorphodynamique ; Roche sédimentaire ; Technique de recherche ; Versant (1)
- Cycle gel-dégel ; Expérimentation ; Géographie physique ; Humidité ; Météorisation ; Roche cristalline ; Technique de recherche (1)
- Eolien ; Fluviatile ; Géographie physique ; Paléo-environnement ; Paléoclimat ; Paléohydrologie ; Pays-Bas ; Périglaciaire ; Quaternaire ; Sédimentologie (1)
- Changing fluvial style of periglacial lowland rivers during the Weichselian Pleniglacial in the eastern Netherlands in Periglacial processes and landforms. (1)
- Frost heaving and frost creep on an experimental slope : results for soil structures and sorted stripes in Periglacial processes and landforms. (1)
- Changing fluvial style of periglacial lowland rivers during the Weichselian Pleniglacial in the eastern Netherlands in Periglacial processes and landforms.
- there was a velocity decrease. This velocity decrease is interpreted as being a consequence of changes in rock elasticity brought about by a diminution in the bonding strength of the rock. This means that wetting, prior to freezing, may weaken a rock.
- the slope and varied in relation to changes in drainage and temperature gradients. The maximum frost creep occurred in the loamy material at the lower end of the slope where the intensity of the water supply and heaving were greater. Frost creep was shown