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Mechanical aspects of postglacial volcanism and tectonics of the Reykjanes Peninsula, southwest Iceland
  • Mechanical aspects of postglacial volcanism and tectonics of the Reykjanes Peninsula, southwest Iceland
Genesis of lateral moraine complexes, demonstrated by fossil soils and trunks| indicator of postglacial climatic fluctuation in Moraines and varves. Origin/Genesis/Classification.
  • Genesis of lateral moraine complexes, demonstrated by fossil soils and trunks| indicator of postglacial climatic fluctuation in Moraines and varves. Origin/Genesis/Classification.
Spät-und postglaziale Gletscherschwankungen in der Ferwallgruppe (Tirol/Vorarlberg). (Late and postglacial fluctuations of glaciers in the Ferwall mountains, western Austria)
  • Spät-und postglaziale Gletscherschwankungen in der Ferwallgruppe (Tirol/Vorarlberg). (Late and postglacial fluctuations of glaciers in the Ferwall mountains, western Austria)
The magnitude and frequency of large rockslides in Iceland in the Postglacial
  • The magnitude and frequency of large rockslides in Iceland in the Postglacial
Human occupation of the submerged coast of the Massif Armoricain and postglacial sea level changes in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
  • Human occupation of the submerged coast of the Massif Armoricain and postglacial sea level changes in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves.
Spätquartäre Sedimentationsgeschichte des Meerfelder Maares (Westeifel). - Mikrostratigraphie jahreszeitlich geschichteter Seesedimente Late Quaternary history of sedimentation in the Meerfelder Maar (Western Eifel). - Microstratigraphy of annually laminated lake sediments
  • This paper describes the history of sedimentation during the last 11.000 years. Using sedimentation rates and the structure of varves it is possible to recognize influences of human activities since neolithic times and even of minor postglacial
Late Weichselian and Holocene sea-level history for a cross-section of western Norway
  • The postglacial sea-level history along a cross-section of western Norway has been studied in detail. Ten local sea-level curves were used to construct an equidistant shoreline diagram, covering the last 13 000 years. This includes 76 radiocarbon
Two mid-Holocene millenia of swamp forest in the Rhine/Meuse deltaic plain
  • The paleoenvironmental evolution of a Dutch deltaic swamp forest area during the mid-Holocene was strongly governed by a general rise of water level (bound to postglacial sea-level rise) and by fluctuations in this water-level rise. A phasing
Snehova pole na ceské strane Krkonos. (Snow patches on the Czech side of Krkonose-Giant Mountains)
  • -1500 m), favourable microclimate and inpart the different rock composition of the beneath the patches. The nivation activity of snow patches contributes to postglacial morphological development.
Quaternary sea-level changes in western Scotland
  • a atteint son maximum entre 6 600 et 7 000 B.P. (Main Postglacial Shoreline).
Late Quaternary shorelines in Ireland: an assessment of their implications for isostatic land movement and relative sea-level changes in Shorelines and isostasy.
  • of a more detailed knowledge of events. Only in postglacial times some basic patterns in Quaternary environmental development have been established. (P. A. Pirazzoli).
Les formations alluviales de l'Allier dans le gisement préhistorique du Blot (Cerzat, Haute-Loire). Eléments de dynamique fluviale. in Colloque AFEQ, Paris 1983. (Alluvial deposits of the river Allier in the paleolithic site of Blot (Cerzat, Haute-Loire, France). Elements of river dynamics)
  • by vertical erosion during the Postglacial Period (post Allerod) which resulted in both the formation of a valley, about ten meters deep, and the throwing up of a lower terrace.