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• W37942328 abstract "AbstractFluvial geomorphic processes (channel and floodplain evolution) are widespread in the extensive lowlands of Hungary. Since flow regulation in the nineteenth century, river channels have shown adjustments of considerable degree. Some agricultural areas in hills and low mountain basins are seriously affected by water erosion, particularly gully development on loess. Although all sand dunes have been stabilized by now, historically wind erosion has also been a major geomorphic agent in blown-sand areas. The areas affected by mass movements and karst processes are limited but their processes still operate – partly in function of the changing climatic conditions. Applied geomorphological research focuses on ever intensifying human impact on the landscape (particularly in mining districts), which has become the primary driver of recent geomorphic evolution in Hungary, too.KeywordsChannel and floodplain evolutionWater erosionLandslidesWind erosionKarstMining impact" @default.
• W37942328 created "2016-06-24" @default.
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• W37942328 date "2011-11-11" @default.
• W37942328 modified "2023-10-12" @default.
• W37942328 title "Recent Landform Evolution in Hungary" @default.
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• W37942328 doi "https://doi.org/10.1007/978-94-007-2448-8_9" @default.
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