inscription
Portail d'information géographique

Résultats de la recherche (1907 résultats)

Affinez votre recherche

Par Collection Par Auteur Par Date Par Sujet Par Titre Par ville ? Par pays ? Par continent ?
  • Aquitaine ; Auto-organisation ; Cordon littoral ; Couplage morphologique ; Dynamique littorale ; France ; Géomorphologie littorale ; Littoral ; Modèle
  • Aquitaine ; Coastal dynamics ; Coastal environment ; Coastal geomorphology ; France ; Model ; Morphological coupling ; Sand bar ; Self-organizing behaviour
  • Double sandbar systems are common morphological features along sandy, wave-dominated, micro- to meso-tidal coastlines. Here the AA. use a numerical model to show that the relative importance of self-organization and morphological coupling changes
  • in favour of the latter with an increase in waterdepth variability along the outer-bar crest. Furthermore, they find that the typical alongshore variability in inner-bar rip-channel scale is indicative of a mixture of self-organization and morphological
  • coupling rather than self-organization alone. Morphological coupling may thus be more important to understanding and predicting the evolution of inner-bar rip channels than previously envisaged.
  • Bassin-versant ; Concept ; Couplage morphologique ; Cône d'éboulis ; Cône de déjection ; Fluviatile ; Montagne ; Niveau de base ; Quaternaire ; Ravinement ; Sédimentologie ; Transport sédimentaire
  • Alluvial cone ; Base level ; Concept ; Debris cone ; Fluvial processes ; Gully erosion ; Morphological coupling ; Mountain ; Quaternary ; Sediment transport ; Sedimentology ; Watershed
  • The implications of coupling relate to downstream channel response, fan morphology, sedimentation patterns and vertical sedimentary sequences. Temporal and spatial scales of coupling are related, and with increasing scales the dominant controls
  • Ciudad Chihuahua : its changing morphology and landscape
  • Mexico ; Suburbanization ; Urban geography ; Urban growth ; Urban morphology
  • Growth and internal spatial dynamics of this state capital and manufacturing center. Suburban expansion and ribbon development since World War II have morphologically transformed Chihuahua. - (DWG)
  • Palaeohydrological reconstructions achieved from palaeoclimatic conditions and palaeochannel morphology for southern Hebei, the North China Plain
  • Dynamics and morphology of the North Branch Ashburton River.
  • The Sheva Shingle beach : a morphological study
  • Some important aspects of the morphological processes in the southwestern United States
  • The morphology of the Aegean Sea: a discussion of morphometrical data
  • Morphology of cobble streams is small watersheds
  • Palsstrukturer och palsmorfologi i Nordnorge Palsa structures and palsa morphology in northern Norway
  • Morphology and relief of Kissonerga village area of Paphos district, Cyprus
  • Morphological properties of the slope profiles of the western plateau scarps, Ranchi
  • Morphology and sediments of sandwaves in the St-Lawrence estuary
  • Dating Quaternary fault scarps formed in alluvium using morphologic parameters
  • Ages of fault scarps, as well as those other types of transport-limited slopes, can be estimated by comparing their morphology with the morphology of scarps of known age. Age estimates are derived by fitting the scarp profiles to synthetic profiles
  • generated using a diffusion equation or, alternatively, by classification using a linear discriminant function. The usefulness of morphology-derived age estimates depends on the relative importance of non-age-related morphologic variation. Data from more
  • than 200 scarp profiles demonstrate that morphologic variation not related to scarp age can introduce significant uncertainties into morphology-derived age estimates.
  • The recreational business district: a component of the East London urban morphology
  • Coastal mudslide morphology and processes on Eocene clays in Denmark
  • The morphology of Johnston and Mansel banks in the Aegean Sea
  • Morphology and development of an alluvial fan in a permafrost region, Aklavik Range, Canada
  • The objectives of this study are to describe the morphology and sedimentology of an alluvial fan, the Mount Goodenough North fan, in a permafrost region; and to interpret the processes responsible for the development of the fan, using both direct
  • observations and inferences from fan morphology and sedimentology.
  • The morphological development of the Wadden Sea Island of Jordsand since the storm surges in 1976
  • Jordsand is the smallest island in the Danish Wadden Sea. In this paper a brief statement of the morphological development of the island is given for the period 1976-88. Furthermore, the development of two adjacent morphological elements, the high
  • A Kozép-békési varosok funkcionalis morfologiai elemzésének altalanosithato tapasztalatai. (Experience to be generalized from the functional-morphological analysis of the mid-Békés towns)
  • The data basis for functional-morphological analyses has considerably broadened (census statistics, etc.). The positions of the mid-Békés towns in the settlement network have changed. Functions modified at a more rapid rate than morphology. (DLO).