inscription
Portail d'information géographique

Résultats de la recherche (22 résultats)

Affinez votre recherche

Par Collection Par Auteur Par Date Par Sujet Par Titre
  • Geomorphology of subtidal and intertidal areas in the Southwest of the Netherlands in Developments in physical geography. A tribute to J. I. S. Zonneveld..
  • In the Southwest of the Netherlands tidal currents are responsible for deposition of subtidal and intertidal sediments in which several characteristic geomorphological units can be distinguished. (AIS).
  • 1983
  • Szeged geomorfologiai vazlata. (Geomorphological sketch of Szeged)
  • 1983
  • Az Eszaki-Bakony elotere és a Pannonhalmi-dombsag domborzata. (Geomorphology of the northern foreland of the Bakony Mountains and the Pannonhalma Hills)
  • The main characteristic of the northern foreground of the Bakony Mountains is that it comprises the mosaic of various geomorphological regions (plain, hilly and mountainous relief types). Alluvial fans of high (250-270 m a.s.l.), medium (150-250 m
  • 1983
  • Krasovy reliéf a jeho vyznam v geomorfologickom obraze Zapadnych Karpat. (Karst relief and its significance in the geomorphological picture of the West Carpathians)
  • 1983
  • 21 years of British geomorphology
  • 1983
  • Geomorfologische kaart van Nederland, Blad 45's-Hertogenbosch.. (Geomorphological map of the Netherlands, Sheet 45's-Hertogenbosch)
  • 1983
  • In the Mountains several generations of geomorphological surfaces are observed, the oldest of which are the covered, exhumed, reshaped, uncovered, buried or semiexhumed horsts. (DLO).
  • 1983
  • Zur weichselzeitlichen Entwicklungeschichte der unteren Saar (Rheinisches Schiefergebirge). Eine geomorphologische und palynologische Untersuchung. (The development history of the Saar River during the Weichselian glaciation. A geomorphological
  • 1983
  • Géomorphologie structurale du batholite de Galway (Connemara, Irlande occidentale). (Structural geomorphology of the Galway batholith (Connemara, Western Ireland))
  • 1983
  • Consecuencias geomorfologicas de las lluvias de noviembre de 1982 en las cabeceras de algunos valles pirenaicos. in Las lluvias catastroficas mediterraneas. (Geomorphological effects of the rainfalls of November 1982 in some Pyrenean headvalleys)
  • 1983
  • is most influenced by the lithology and geomorphology, climatic conditions and consequences of a paleopotamological development of large rivers. (MS).
  • 1983
  • The geomorphological, lithostratigraphical, paleontological and paleomagnetic data were considered together for the profile of the Gyongyosvisonta open cast lignite mine pit. (DLO).
  • 1983
  • Four regions differing in slope conditions (the plain and alluvial fan zone, the Pannonhalma Hills, the northern foreland of the Bakony and the mountainous part of the Bakony) are differentiated and described geomorphologically. (DLO).
  • 1983
  • Investigations of the eastern part of the Rhine glacier area of the Würmian glaciation (Rotach and Argen lobes). The geomorphology has been studied specially from a regional-historical, the sedimentology mainly from a thematical point of view. (AIS).
  • 1983
  • The 100th anniversary of author's birth is celebrated by the publication of his results achieved during fifty years of research. The distribution of salt-affected soils on the Danube-Tisza Interfluve, its geomorphological and hydrological reasons
  • 1983
  • The north shore sloping flats of the Lake Balaton aera are considered landscape typologically a moderately dissected piedmont surface with rendzinas and locally various zonal soils and a deep groundwater table. Its lithology, geomorphological
  • 1983
  • Field and laboratory investigations into the sedimentology and geomorphology of thick stratified slope deposits (grèzes litées) in the Rothaargebirge, in the northeastern part of the Rhenish Slate Mountains show that these deposits were formed
  • 1983
  • Geomorphology and sedimentology. Description of the river from Pleistocene over Younger Dryas, Preboreal, Atlantic up to historical times (13th century). Influence tidal activity, dikes systems, sea level and inundations. (LW).
  • 1983
  • As appears from geomorphological and palynological data, the Heerenven lake in the nature reserve De Hamert forms a remnant of a branch of the river Meuse, dating from the Weischselian Glacial Period.
  • 1983
  • The geomorphological and morphotectonical study of the alluvial terraces in the subalpine region of Digne (Alpes de Haute-Provence-France) clearly shows an important pleistocene tectogenic phase. This one is post the subalpine overthrust which takes
  • place during the upper Neogen. This quaternary tectonic phase had important effects on the geomorphological evolution of the Bleone river basin.
  • 1983