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Par Collection Par Auteur- KAPUR, S. (1)
- SARI, M. (1)
- SENOL, S. (1)
- DINC, U. (1)
- ZUIDAM, R. A. van (1)
- Geography of Asia (4)
- Aridité ; Climatologie ; Domaine aride ; Donnée climatique ; Désert ; Ecosystème ; Géographie de l'Asie ; Indice d'aridité ; Israël ; Negev ; Propriété physico-chimique ; Précipitation ; Sol (1)
- Carte géomorphologique ; Cartographie thématique ; Géographie de l'Asie ; Géologie régionale ; Géomorphologie appliquée ; Hydrologie appliquée ; Indonésie ; Jawa ; Pédologie ; Rembang ; Semarang (1)
- Catena ; Cukurova région ; Delta ; Domaine méditerranéen ; Géographie de l'Asie ; Littoral ; Néotectonique ; Propriété du sol ; Pédologie ; Sol ; Turquie ; Turquie du Sud (1)
- Cordon littoral ; Cénozoïque ; Dune ; Géographie de l'Asie ; Indonésie ; Jawa ; Lithologie ; Littoral ; Niveau marin ; Paléosol ; Quaternaire zone chaude ; Tectonique ; Variation climatique ; Volcanisme (1)
- Applied geomorphological mapping of Indonesia (1)
- Catenary soil relationships in the Cukurova region, southern Turkey (1)
- Climatic and non-climatic controls of aridity : the case of the northern Negev of Israel in Arid and semi-arid environments. Geomorphological and pedological aspects. (1)
- Late Tertiary and Quaternary coastal landscape development of the Kroya Beach Ridge area (south central Java, Indonesia) (1)
- Climatic and non-climatic controls of aridity : the case of the northern Negev of Israel in Arid and semi-arid environments. Geomorphological and pedological aspects.
- The aim of this study is to produce a comparative basic pedological concept of the soils of the region in a catenary sequence. The catena studied is typical for the Mediterranean coastal areas covering surfaces, geomorphic units, formed
- by neotectonic activity and the following processes related to pedology.
- territory, and the programme can be regarded as an example of a survey applicable to environmental planning and management as well as to the standard geological, pedological and hydrological surveys. (AIS).
- Topographical, lithological and paleo-pedological features enable the reconstruction of the Late Tertiary and Quaternary development of the Kroya coastal plain. Climatic changes and sea-level fluctuations during the Pleistocene, and tectonic