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  • A Kisalfold muholdas foldtudomanyi vizsgalata. (An analysis of the Little Plain of earth sciences viewpoint from satellite images)
  • Information from the processing of LANDSAT-1,-2 and-3 images is interpreted to delimit the Little Plain and compared with the data/on relief, drainage, surficial geology, groundwater conditions, soil erosion and deep geology/accumulated by decades
  • The extent of some glaciers in Northern Iceland during the little ice age and the nature of recent deglaciation
  • Lichenometric studies from four glaciers in Northern Iceland are used to determine the dates of their Little Ice Age maxima. In all cases these date to the last half of the nineteenth century and probably marked the maximum Neoglacial extent
  • 14C dating and paleoenvironment of the historic Little Ice Age glacier advance of Nigardsbreen, Southwest Norway
  • A large settlement in the Little Hungarian Plain. Its historical description is followed by the new age development, which induced changes in functional morphology, too. - (JS)
  • The A. gives an historical background and a modern economical appraisal of the Kiel Canal as one of the most important waterways of the world that had little impact on Kiel and its commerce. (L'éd.).
  • Little ice age flooding in the Ivalojoki and Oulankajoki valleys, Finland ?
  • The A. discusses the distinctive demographic trends among Soviet Moslems, whose numbers are projected to rise from 44 million in 1979 to 64 million in the year 2000. This group is distinguished by high rates of natural increase, little mobility
  • regressions. The examination of the 10 control variables has little influence in modifying the autonomous dynamics of the model. (INRA).
  • Although there is a debate about the alleged significance of changes in farm occupancy to the management of the farmed landscape, there is little empirical research detailing the relationships. With use of a longitudinal analysis of over 250 farm
  • The features of settlements transformation in Fergana valley and Khorezm oasis are considered. Poor reserves of territorial-economic development, little migrational mobility and prevailence of rural population, low level of urbanization
  • of rivers known to flod regularly over two twenty year periods. During the first period, 1940-1959, there was still little regulation of the rivers and ditching of the forests and bogs| during the second period, 1964-1983, the changes wrought by man were
  • are insignificant. No little ice age till 1850, no warning since this date. We have tried to explain the stability of climate in this province by an increase of oceanic tendancy. (The Author).
  • | the rapidly renewable groundwater resources of the Little Plain are now probably the most significant and there is no hope to improve surface and groundwater quality for ensuring drinking water supply. - (DLO), (JS)