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  • The Holocene development of the Young Coastal Plain of Suriname
  • A new series of 19 radiocarbon dates from the Holocene Young Coastal plain in Suriname fits into the picture of a rapid sea-level rise in this area until about 6000 B.P. From 6000 B.P. onward the sea-level remained essentially at its present
  • position. Indication for a higher position of the sea-level at about 6500 B.P. are inconclusive. From about 6500 B.P. onward the marine influence in the interior part of the Young Coastal Plain diminished, but some marine oscillations were registered
  • . The available evidence is too limited to permit pertinent conclusions about the regional occurrence of marine fluctuations. From an analysis of the younger Holocene development in the Hertenrits area it is concluded that a new subdivision has to be established
  • 1978
  • Bükk Mts can be classified as young formation of Alpine structural features and shows the pecularities of denuded plateaus and block-mountains composed by sedimentary, igneous and eruptive rocks and ophiolites. (CK).
  • 1978
  • Jungquartäre Relief-und Bodenentwicklung im Küstenbereich Südwestmarokkos. (Young Quaternary relief and soil development in the coastal area of southwestern Morocco)
  • 1978
  • Kartometryczne metody wyznaczania zasiegu form m odoglacjalnych na przyk adzie Wysoczyzny Kolnenskiej. (Cartometric methods in determining the extent of young-glacial forms. A case study of the Kolno Upland)
  • 1978
  • YOUNG, E. W.
  • 1978
  • of participants for the project, strengthened the position of the married men as opposed to that of women and of younger men, and favoured the larger, wealthier and powerful concessions. Althought the social stratification in its main characteristics remained
  • 1978
  • at 4000 m within the glaciated area. This date is slightly younger than those from similar altitudes on other equatorial mountains.
  • 1978
  • First stages of relief transformation of the young uplifted mountains
  • 1978
  • the colonial time have reinforced the position of the elders and increased socio-economic inequality. However, the young are no longer prepared to suffer gerontocracy and escape from it through out-migration. The decline of the traditional power groups may
  • 1978
  • borings and geophysics. The distribution of the Neogene volcanism as well as the thin crust and high heat flow found by these investigations revealed however the existence of an active young-alpine mantle arch. The area above the mantle arch subsides
  • 1978