Health pattern of the rural people in Lower GangaPlain
Activité professionnelle ; GangaPlain ; Inde ; Niveau d'instruction ; Population rurale ; Santé ; Structure démographique ; Structure sociale
This paper focuses on the health pattern of rural population in the Lower GangaPlain (eastern India). Author accomplished an analysis of health conditions of the local population according to demographic structure (age and sex), social composition
Territorial organization of settlements in a part of the GangaPlain, India
Ganga, fl. ; Géographie de l'Asie ; Géographie historique ; Habitat rural ; Histoire du peuplement ; Inde ; Organisation de l'espace ; Peuplement ; Plaine ; Village
Histoire du peuplement dans la plaine du Gange et leur inscription dans l'organisation de territoires des clans jusqu'au XIV siècle. La transition jusqu'à nos jours et l'identification des principales phases d'organisation territoriale des unités de
Oxygen isotopes of bovid teeth as archives of paleoclimatic variations in archaeological deposits of the GangaPlain, India
Datation C 14 ; Dent ; Ganga ; Géochimie ; Holocène ; Inde ; Mammifère ; Oxygène 18 ; Paléo-environnement ; Paléoclimatologie ; Plaine alluviale ; Site archéologique ; Variation climatique
Alluvial plain ; Archeological site ; C 14 dating ; Climatic variation ; Ganges River ; Geochemistry ; Holocene ; India ; Mammal ; Oxygen 18 ; Palaeo-environment ; Palaeoclimatology
The AA. have made an attempt to interpret climatic variations during the past 3600 yr using oxygen isotope data from teeth enamel from archaeological sites in the central alluvial plain of the Ganga river. This is the first record of climatic
variability in the Gangaplain during this time frame.
Geomorphology, pedology and sedimentology of the Deoha/Ganga-Ghaghara Interfluve, Upper Gangetic Plains (Himalayan Foreland Basin) - extensional tectonic implications
Cartographie ; Datation ; Ganga ; Inde ; Micromorphologie ; Néotectonique ; Paléosol ; Plaine alluviale ; Propriétés du sol ; Sol ; Thermoluminescence
Alluvial plain ; Cartography ; Dating ; Ganges River ; India ; Micromorphology ; Neotectonics ; Palaeosol ; Soil ; Soil properties ; Thermoluminescence
The Deoha/Ganga-Ghaghara Interfluve has been mapped for its geomorphology, and soil-geomorphic units, tectonic features, using remote sensing digital data analysis and geographical information system techniques. Also, fieldwork was carried to study
Geomorphic characterization and diversity of the fluvial systems of the Gangetic plains
Bihār ; Bilan sédimentaire ; Cours d'eau ; Ganga ; Géomorphologie ; Hydrodynamique ; Inde ; Néotectonique ; Plaine alluviale ; Plaine d'inondation ; Régime hydrologique ; Transport sédimentaire ; Uttar Pradesh
Alluvial plain ; Bihar ; Floodplain ; Ganges River ; Geomorphology ; Hydrodynamics ; Hydrological regime ; India ; Neotectonics ; Sediment budget ; Sediment transport ; Stream ; UttarPradesh
The AA. select 2 regions of the Gangetic plains to compare the morphology, hydrology, and fluvial processes : the Ganga-Yamuna interfluve in the Western Gangetic Plains (WGP) of Utar Pradesh and the Gandak-Kosi interfluve in the Eastern Gangetic
Plains (EGP) of north Bihar. The aim of this paper is to investigate the spatial inhomogeneity across the plains and to explain any diversity in terms of geomorphic and geologic controls.
Institutional forces behind water conflict in the Gangaplains
Bangladesh ; Barrage ; Bassin fluvial ; Bihār ; Conflit ; Coopération internationale ; Environnement ; Ganga ; Gestion ; Gestion de l'eau ; Inde ; Marginalité ; Népal ; Région périphérique
L'A. présente les conflits portant sur l'eau dans la plaine indienne du Gange. L'Etat du Bihar (capitale Patna), ne peut pas convaincre le gouvernement fédéral de Delhi d'établir une meilleure gestion de l'eau. Patna craint également que la
(PZ) of the western GangaPlain. A large alluvial fan and incised river valley surfaces with numerous cut-off channels/palaeochannels are the main landforms of the area. The proximal basin margin, against the Himalaya mountain range, is defined
Geomorphic and tectonic features in a part of the Piedmont Zone (PZ) of the west GangaPlain have been identified and mapped on the basis of various terrain characteristics and sedimentological attributes using Digital Terrain Models, remote sensing
Evolution of the Lower Gangetic Plains landforms and soils in West Bengal, India
Argile minéral ; Cartographie ; Fer ; Ganga ; Inde ; Niveau marin ; Néotectonique ; Plaine ; Propriétés du sol ; Pédogenèse ; Sol ; Sol hydromorphe ; West Bengal
Cartography ; Clay mineral ; Ganges River ; Hydromorphic soil ; India ; Iron ; Neotectonics ; Pedogenesis ; Plain ; Sea level ; Soil ; Soil properties ; West Bengal
The objectives of this study were : 1) identification and mapping of different landforms and soil-geomorphic units in the Lower Gangetic Plains of West bengal, and construction of a soil chrono-association for the area; 2) deciphering the major soil
Polygenetic soils of the north-central part of the Gangetic Plains : a micromorphological approach
Argile minéral ; Carbonate ; Ganga ; Holocène ; Inde ; Micromorphologie ; Météorisation ; Plaine gangétique ; Propriétés du sol ; Pédogenèse ; Uttar Pradesh ; Variation climatique
The AA. use micromorphological, physical, chemical, and mineralogical analyses to determine the polygenetic nature of soils on the Gangetic Plains. Micromorphology helps to distinguish pedogenic and nonpedogenic features, older and younger clay
Ganga ; Inde ; Micromorphologie ; Paléoclimatologie ; Paléosol ; Plaine alluviale ; Propriétés du sol ; Pédogenèse ; Quaternaire
Alluvial plain ; Ganges River ; India ; Micromorphology ; Palaeoclimatology ; Palaeosol ; Pedogenesis ; Quaternary ; Soil properties
Micromorphological examination of the paleosols developed in alluvial fan deposits of the NW Himalayas and the bordering polygenetic soils (mainly Holocene) of the Gangetic Plains has been used to differenciate the pedosedimentary features
Role of microtopography in the formation of sodic soils in the semi-arid part of the Indo-Gangetic Plains, India
Domaine aride ; Domaine semi-aride ; Ganga ; Inde ; Micromorphologie ; Microtopographie ; Minéralogie ; Néotectonique ; Plaine alluviale ; Propriétés du sol ; Punjab ; Pédogenèse ; Sol salin ; Sol sodique ; Uttar Pradesh
Alluvial plain ; Arid area ; Ganges River ; India ; Micromorphology ; Mineralogy ; Neotectonics ; Pedogenesis ; Saline soil ; Semi-arid area ; Soil properties ; UttarPradesh
In the northwestern part of the Indo-Gangetic Plains (IGP), India, non-sodic and moderately sodic soils occur on microhigh (MH) and highly sodic soils on microlow (ML) position under a semi-arid climate. The main soil-forming processes have been
Geomorphologic map of the R. Brahmaputra-Jamuna and R. Ganges plain En japonais
Aménagement hydraulique ; Barrage ; Brahmaputra, plaine ; Carte géomorphologique ; Cartographie thématique ; Cours d'eau ; Ganga, plaine ; Géographie de l'Asie ; Inde ; Localisation ; Photointerprétation ; Technique cartographique ; Télédétection
Cartographie de la plaine du Brahmapoutre et du Gange à partir de photographies ERTS, des photographies aériennes et des relevés de terrain. Le but de ce travail étant de définir un site de barrage. Parmi plusieurs sites possibles, l'A. préfère
This paper concerns with the morphometry of the flood plains. Against the general conception that a flood plain widens from upstream to downstream, the AA. point out that, at least in the Moldavian Tableland, the width of a flood plain increases
only together with the increase of Strahler order; moreover, between two successive confluence of the same or of close orders, a flood plain narrows from upstream to downstream, being regenerated by a new confluence. This tendance is a general rule
in the Moldavian Tableland, and seems to have a large extension in the Romanian flood plains. - (E. Rusu).
The Coghinas coastal plain is an alluvial plain in a half-graben structure where three different zones are morphologically divided. On the basis of the criteria followed in this investigation, the climatic data, the comparison between historical
maps (since the 1841), the fluvial evolution suggest a discontinue and disuniform sedimentation related to the inner plain. - (NF)
The five distinct topographic units of the vicinity of the town (alluvial plain covered with wind-blown sand, Upper Pleistocene residual levels, high flood-plain, low flood-plain and the active flood-plain) are described and mapped by the author.