Solr Search · GéoProdig, portail d'information géographique

Geomorphological and paleohydrographical research based on geoelectrical prospection (South Campine, Belgium)
1981

A geomorphological profile, Hedemarken, Norway
made it possible to distinguish between different landforms, to define geomorphological units as landforms of second order and to classify geomorphological regions. (IMB).
1981

Geomorfologia Podhradskej kotliny. (Geomorphology of the Podhradska Kotlina Basin)
Regional geomorphological analysis of a typical erosive and faultly delineated basin of Eastern Slovakia. It represents an inverse formation formed through erosion-denudation processes on a strup of less resistent flysch with sandstone-claystone
1981

Fresh and salt groundwater in the Dutch coastal area in relation to geomorphological evolution
Historical sequences of encroaching seawater and recharge of fresh water under different geological and geomorphological conditions during the Quaternary are responsible for a rather complicated distribution of fresh and salt groundwater
1981

Geomorfologické pomery Borskej niziny. (Geomorphological conditions of the Borska nizina lowland)
1981

Geomorfologie chranené krajinné oblasti Kokorinsko a prilehlého uzemi. (The geomorphology of the protected landscape area Kokorinsko and the adjacent area)
1981

This study is a geomorphological and pedological contribution to an interdisciplinary survey of landscape eclogy of the Dutch coastal dunes. The relationship between climatic history, coast development and geology are described and human influences
on the dune area in the past. A comprehensive classification of coastal dune forms is given as used for geomorphological maps, a map scale 1:100 000 is enclosed. Some attention is given to actual processes. The causes of the sudden formation of the Younger
1981

Complex analysis of the Lower Zitava river terraces and their geomorphological and geological-stratigraphical characteristics. (MS).
1981

To evaluate the importance of anthropogenous changes of the relief it is necessary to consider the further geomorphological development of new forms and the possibility of their economic application. Cartographic methods of interpretation. (MS).
1981

for a correlation between the depth structure and geomorphology. It is a discussion of examples, which shows that the geomorphological elements (marginal zones of Weichsel ice period, relief of sea ground and position of coastal line) are influenced by these depth
1981

The AA., on the basis of their recent geomorphological studies, consider Lake Balaton to be a polygeneous depression formed by sinking periodical both in space and time. Its slow sinking started in the Riss, became more active in the Würm, mainly
1981

New geomorphological aspects in the Brno surroundings. In the pocket-like depressions had a great importance the intensive tectonic skattering of platform basement rocks, conditioned by ancient tectogeneses and by deep faults. (MS).
1981

Geomorphological and geological investigations on closed topographic depressions and valley systems on the Drente plateau allow correlations to be made between the location of pingo remnants on the plateau and the Weichselian drainage pattern
1981

The possibilities of using multispectral space photographs in investigating the tectonic structure and geomorphology of the West Carpathians. The work is focused to the analysing of basic structures of Middle Slovakian neovolcanits. (MS).
1981

A complex investigation of the evolutional history of the blown-sand area is undertaken by stratigraphic, pedologic, palynologic methods, radiocarbon dating and recent geomorphological observations. The fossil soils found indicate blown-sand
1981

Der Sedimenthaushalt der Ruhr. in Beiträge zur angewandten Geomorphologie-Contributions in applied geomorphology. (Le budget sédimentaire de la Ruhr)
1981

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