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- > DUGMORE, A.J. (supprimer)
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Par Collection Par Auteur- DUGMORE, A.J. (2)
- HOLMGREN, Karin, (Auteur des parties liminaires) (1)
- THOMAS, M.F., (Editeur scientifique) (1)
- THOMSON, A. (1)
- VÉSTEINSSON, O. (1)
- SIMPSON, I.A. (1)
- SMITH, K.T. (1)
- Action anthropique ; Dégradation de l'environnement ; Ecologie humaine ; Erosion des sols ; Géographie historique ; Islande ; Modélisation ; Politique agricole commune ; Surpâturage ; Téphrochronologie ; Utilisation agricole du sol (1)
- Agricultural land use ; Common agricultural policy ; Environmental degradation ; Historical geography ; Human ecology ; Human impact ; Iceland ; Modelling ; Over-grazing ; Soil erosion ; Tephrochronology (1)
- C 14 dating ; Glacial surge ; Holocene ; Human occupation ; Iceland ; Quaternary ; Sandur ; Sedimentology ; Tephrochronology (1)
- Crue glaciaire ; Datation C 14 ; Holocène ; Islande ; Occupation humaine ; Quaternaire ; Sandur ; Sédimentologie ; Téphrochronologie (1)
- Climate-human society interactions during the Holocene (1)
- Crossing the thresholds : human ecology and historical patterns of landscape degradation (1)
- Jökulhlaups circa Landnám : mid- to late first millennium AD floods in South Iceland and their implications for landscapes of settlement (1)
- Landscape sensitivity : principles and applications in northern cool temperate environments (1)
- Agricultural land use ; Common agricultural policy ; Environmental degradation ; Historical geography ; Human ecology ; Human impact ; Iceland ; Modelling ; Over-grazing ; Soil erosion ; Tephrochronology
- observation of soil erosion, temporally defined by tephrochronology, to highlight the extent of land degradation during this period. The tragedy of the commons explanation of degradation is then assessed by evaluating historic documentary sources
- C 14 dating ; Glacial surge ; Holocene ; Human occupation ; Iceland ; Quaternary ; Sandur ; Sedimentology ; Tephrochronology
- ), the most recent prehistoric events in a series of Holocene floods in the Markarfljót valley, are securely dated by tephrochronology and radiocarbon dating to between c. AD 500 and c. AD 900. The environmental impact of these events would have been extensive