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  • Pleistocene geology and geomorphology of the Smoking Hills Upland and lower Horton River Arctic coast of mainland Canada
  • Arctique ; Canada ; Glaciaire ; Géographie de l'Amérique ; Interglaciaire ; Paléo-environnement ; Pléistocène ; Quaternaire ; Réseau de drainage ; Smoking Hills Upland
  • The purpose of this paper is to discuss the Pleistocene landforms and associated deposits that could shed light on the glacial history of the Smoking Hills Upland and lower Horton River area.
  • 1989
  • Environmental deterioration in the hill-country of Sri Lanka
  • 1989
  • Aspects of the Quaternary in the Tertiary Hills of Bavaria in Landforms and landform evolution in West Germany.
  • 1989
  • Frontier settlement and landlessness among hill migrants in Nepal Tarai
  • 1989
  • Davis Creek silt, an early Pleistocene or late Pliocene deposit in the Cypress Hills of Saskatchewan
  • 1989
  • Vegetationsveränderung in Grünland einer Flussaue des Sachsischen Hügellandes durch Nutzungsintensivierung Vegetation change in the grassland of a river flood plain in the Saxon hill country caused by intensified land use
  • 1989
  • Massive reforestation in two hill districts over the past 24 years belies the generalization of a denuded Nepal. - (DWG)
  • 1989
  • Upper Siwalik palaeoenvironments and palaeoecology in the Pabbi Hills, northern Pakistan
  • 1989
  • Les versants à banquettes de Ronas Hill. Essai de définition d'une province périglaciaire aux îles Shetland in Régions arctiques et subarctiques.
  • 1989
  • More than 500 landslides were analyzed in relation to angle of hill-slope, lithology, vegetation and road construction. - (DWG)
  • 1989
  • In this paper, a method of assessing the spatial variation of the solute loads of different subcatchments is presented, using a catchment in the Tertiary Hills of Bavaria as an example.
  • 1989
  • Consideration of the structure and morphology of the study area as a whole, as well as that of a small constructional volcanic hill suggests that it evolved in two phases. The principal phase of development involved a period of crustal extension
  • 1989
  • the Quaternary new slopes were formed as the highland due to volcanic processes, erosion of antecedent valleys and river piracy, glacial processes (slopes of cirques, troughs and morainic hills). Climatic change controlled the type and rate of slope processes
  • 1989
  • time. Traces of glacial erosion are distinct in the Kandalaksha Bay, central depression and near the Karelian coast, the ice moved from NW. Various glacial and glaciofluvial hills and depression are mapped on the floor of the Onega Bay, as well
  • 1989
  • l'importance de Nuwara Eliyas comme hill station , de la morphodynamique récente des côtes, des forêts des hauts plateaux de l'Est ainsi que de la propagation de la malaria dans l'île. Le dernier article mentionne les causes écologiques de l'existence et de la
  • 1989