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  • Palaeohydrologic conditions in the Mark River basin during the last 15.000 years
  • Action anthropique ; Belgique ; Datation C 14 ; Fluviatile ; Géographie physique ; Mark rivière ; Paléogéographie ; Paléohydrologie ; Plaine d'inondation ; Quaternaire ; Stratigraphie ; Structure sédimentaire ; Sédimentation ; Variation climatique
  • This paper presents an outline of lithologic and morphologic developments in the alluvial environment of the Mark Basin in Central Belgium during Post Glacial times. By means of about 900 borings the spatial arrangement and stratigraphic position
  • of palaeomorphologic features and sedimentary units in different parts of the basin was reconstructed. This, together with the radiocarbon datings, offers an insight into Holocene palaeohydrologic conditions in the Mark River floodplain. The influence of prevailing
  • 1989
  • Textural features of fluvial and aeolian deposits in the Mark River valley (Belgium)
  • Belgique ; Eolien ; Fluviatile ; Glaciaire ; Granulométrie ; Géographie de l'Europe ; Mark vallée ; Minéraux lourds ; Morphoscopie ; Paléo-environnement ; Quartz ; Quaternaire ; Sédimentologie ; Vallée
  • The valley of the river Mark (Belgium) is filled with deposits of fluvial and aeolian origin accumulated during the Pleniglacial or the beginning of the Late Glacial, not later than 12.000 yr BP. The aim of the investigations was to determine those
  • 1989
  • Identification of an ancient glacier marks using AVHRR imagery in Special issue : Applications of AVHRR data.
  • 1989
  • Mark Twain in the geography classroom : should we invite him in?
  • 1989
  • In this study, analysis of total sulphur contents of conifer needles reveals marked patterns that are correlated with modelled atmospheric concentrations of sulphur dioxide. Correlations with other indices of sulphur pollution, including wet and dry
  • 1989
  • , spanning a period of marked interannual variability of the atmospheric circulation and sea ice (1977-83) are analyzed using sets of DMSP (Defense Meteorological Satellite Program) imagery.
  • 1989
  • is marked. As a result sand evacuation from the sandy desert regions to the adjacent territories (prebbly and clayey planes) is weakened. - (L'A.).
  • 1989
  • ) and are designated as Early and Late African respectively. Since Miocene a post-African pediplain formation begins which marks the epoch of global pediplanation. The process proceeded along with erosion and alluviation in river valleys. Early Africain surface
  • 1989
  • on 38 m abs. mark and its flowage and freshening by 2005 year. It will slop salinization of residual basin and restore its function as a regional salt receiver. Use of planning water tributaries on the whole area of water has not such effect. So
  • 1989
  • The work is divided in nine chapters : 1- The Genesis of Burma, 2- British occupation, 3- Independent Burma, 4- Period of parliamentary democracy, 5- Independant Burma : second phase to date, 6- Major land marks of the military regime, 7
  • 1989