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Geomorfologické pomery Cachtickych Karpat s osobitnym zretelom na Cachticky kras. (The geomorphological conditions of the Cachtice Carpathians with special regard to the Cachtice Karst)
The Cachtice Carpathians relief and in their framework the Cachtice Karst represent a collection of structural, tectonic, erosion-denudation, karst, fluviokarst, erosion-accumulation and anthropogenous forms. The geomorphological evolution can
1979

Regionalizacia geomorfologickych celkov CSSR z hladiska potencialnej erozie lesnej pôdy. (Regional categorization of Czechoslovak geomorphologic units on the basis of a potential erosion of forest soils)
Important data on potential erosion of forest soils by running water are summarized in all 177 geomorphological units in Czechoslovakia. The Frevert-Zdrazil method of erosion calculation modified by O. Stehlik is applied. The erosion intensity may
1979

Considerations on the relations between landforms, sediments and genesis at ice margins of the Würm Maximum based on geomorphological mapping in the area of the former Iller Glacier (Allgäu/Bavaria) in Moraines and varves. Origin/Genesis
1979

An overall review of the dutch coastal dune area has been given. In spite of the fact that this area, in geomorphological as well as in ecological respect, is one of the best preserved landscapes of the Netherlands many changes have occurred since
1850. Some of the changes have natural causes, most changes were induced by man. Maps on a scale 1:100.000 indicate the present ecological, geomorphological, hydrological and vegetational situation as well the changes in the period 1850-1970. (ALS).
1979

In this study modern is the landscape typological terminology, which is applied instead of the earlier geomorphological denominations. This new complex terminology, taking into consideration the Hungarian landscape terminology (Pécsi, Jukucs 1972
1979

The disturbances of the wind through geomorphological influences are studied according to measurements of the wind velocity and wind directions in two selected meteorological stations in the High Tatras. The results are statistically evaluated
1979

of the history of geomorphological and tectonical development of the young mountain. (CK).
1979

The geomorphological and bioclimatological conditions of Plzen agglomeration is unfavourable in comparison with other large towns in Czechoslovakia. In the Plzen basin are frequent inversions of temperature, and fogs decrease the annual sum
1979

Siedlungsräumen. Festschrift zum 42. Deutschen Geographentag in Gottingen, 1979.. (Patterns of geomorphological structure of the lower Saxonian Mountains in interdependence tectonic, halokinesis, resistence conditions and drainage systems)
1979

The geomorphological significance of the Wolstonian glaciation of eastern England
1979

soils more or less bleached, rubefied and encrusted after the geochimical environment characteristics and the topographical age. The geopedological map sums up the data usually given by a geomorphological map and a pedological map. It underscores
1979

Total amplitudes of neotectonic movements are usually calculated without taking into consideration the Cenozoic lowering of the World Ocean level, which results in grave errors in views on tectonics and geomorphology, as the value of the lowering
1979

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