. "1"^^ . "0169-555X" . "NL - Nizozemsko" . "11"^^ . . "17310" . "1"^^ . . "RIV/61988987:17310/14:A1401A6Y" . "Chronology of processes in high-gradient channels of medium-high mountains and their influence on alluvial fans properties" . . . "dendrogeomorphology; alluvial fan; debris flow; flood; The Moravskoslezsk\u00E9 Beskydy Mts"@en . "Chronology of processes in high-gradient channels of medium-high mountains and their influence on alluvial fans properties"@en . . "\u0160ilh\u00E1n, Karel" . . . "\u00FAnor" . "RIV/61988987:17310/14:A1401A6Y!RIV14-GA0-17310___" . . "[A763D5E1A951]" . "High-gradient channels are the locations of the greatest geomorphological activity in medium-high mountains. The channels' frequency and character influence the contemporary morphology and morphometry of alluvial fans. There is currently no detailed information regarding the frequency of these processes in high-gradient channels and the evolution of alluvial fans in medium-high mountains in Central Europe. This study in the Moravskoslezsk\u00E9 Beskydy Mts. analysed 22 alluvial fans (10 debris flow fans and 12 fluvial fans). The processes occurring on the fans were dated using dendrogeomorphological methods. A total of 748 increment cores were taken from 374 trees to reconstruct 153 geomorphological process events (60 debris flow and 93 floods). The frequency of the processes has been considerably increasing in the last four decades, which can be related to extensive tree cutting since the 1970s." . . . . "7259" . . "GEOMORPHOLOGY" . "206" . . "High-gradient channels are the locations of the greatest geomorphological activity in medium-high mountains. The channels' frequency and character influence the contemporary morphology and morphometry of alluvial fans. There is currently no detailed information regarding the frequency of these processes in high-gradient channels and the evolution of alluvial fans in medium-high mountains in Central Europe. This study in the Moravskoslezsk\u00E9 Beskydy Mts. analysed 22 alluvial fans (10 debris flow fans and 12 fluvial fans). The processes occurring on the fans were dated using dendrogeomorphological methods. A total of 748 increment cores were taken from 374 trees to reconstruct 153 geomorphological process events (60 debris flow and 93 floods). The frequency of the processes has been considerably increasing in the last four decades, which can be related to extensive tree cutting since the 1970s."@en . "Chronology of processes in high-gradient channels of medium-high mountains and their influence on alluvial fans properties" . . . . "Chronology of processes in high-gradient channels of medium-high mountains and their influence on alluvial fans properties"@en . . "P(GAP209/10/0309)" .