Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
EOLIC SEDIMENTS IN WESTERN CARPATHIANS, THEIR CHARACTERIZATION AND CHRONOSTRATIGRAPHY
Loesses in Western Carpathians cover the area of 7 000 square kilometres. The difference of paleographic relations between Eastern and Western Slovakia during the course of Pleistocen is reflected in their morphology, litotype, physical, chemical, and geocnemic properties, in the composition of extraction minerals, in the content of CaCO3, in the character of malacofauna, and the typology of fossile soils. To achieve the thickness of l-5-20 m, a maximum thickness being 35 to 40 m. Eolic sands can be found in the Záhorská nížina lowlands, Podunajská rovina flatland, and East-Slovakian lowland. Morphologically, they form 5-20 m high piles of parabolic and longitudinal form. Winds from various directions were active in their formation. The association of extraction minerals proves that these had been blown out from neogene sediments of the nearby vicinity and from river sediments of the Morava, Danube, and Tisa rivers and their tributaries.
EOLIC SEDIMENTS IN WESTERN CARPATHIANS, THEIR CHARACTERIZATION AND CHRONOSTRATIGRAPHY
Loesses in Western Carpathians cover the area of 7 000 square kilometres. The difference of paleographic relations between Eastern and Western Slovakia during the course of Pleistocen is reflected in their morphology, litotype, physical, chemical, and geocnemic properties, in the composition of extraction minerals, in the content of CaCO3, in the character of malacofauna, and the typology of fossile soils. To achieve the thickness of l-5-20 m, a maximum thickness being 35 to 40 m. Eolic sands can be found in the Záhorská nížina lowlands, Podunajská rovina flatland, and East-Slovakian lowland. Morphologically, they form 5-20 m high piles of parabolic and longitudinal form. Winds from various directions were active in their formation. The association of extraction minerals proves that these had been blown out from neogene sediments of the nearby vicinity and from river sediments of the Morava, Danube, and Tisa rivers and their tributaries.
EOLIC SEDIMENTS IN WESTERN CARPATHIANS, THEIR CHARACTERIZATION AND CHRONOSTRATIGRAPHY
Košťálik Ján (Autor:in)
1997
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
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