Channel processes in the rivers of mountains, foothills and plains
Chalov R., Kamykowska M., Krzemień K. (red), 2006, Channel processes in the rivers of mountains, foothills and plains, Prace Geograficzne, z. 116.
Język publikacji: angielski
Human impact on the hydrological regimen and fluvial processes of the River Wda
Changes in geomorphology of new shoreline after the filling of the Włocławek artificial lake
Hydraulic resistance in river channels and its relationship TO channel processes
Catastrophic earthquakes in the Altai Mts, their aftermath and impact on slope and fluvial processes
The river Katun, its channel morphology and changes due to river engineering and alluvium extraction
Comparative analysis and typology of channel processes in mountain, foreland and flatland rivers
On the evolution of a foreland river network
Navigation on the tailwaters of the Nizhny Novgorod hydropower dam on the River Volga
The geomorphological effects of flash floods in mountain river channels. the case of the River Wilsznia (western Carpathian mountains)
Deltas in dam-retained lakes in the Carpathian part of the Vistula drainage basin
Patterns in foreland fluvial processes
Summary: Foreland and mountain river channels differ markedly in terms of gradient, bedload composition and channel type as a result of differing geology and development processes in these two environments. To understand these differences, a comparison was made between the foreland rivers of the Northern Caucasus and the Western Ural Mountains. The foreland rivers selected represent the type of fluvial process characteristic for areas just below mountains, where the bedload is deposited and channels start branching out. The Western Ural rivers are peculiar in having developed flatland type channels while still within the mountains and meandering channels upon entering mid-mountain plains. This diversity of fluvial processes can be attributed to differences in geotectonic movements between the mountains and the foreland. Indeed, in the Caucasus, these have different directions and high amplitude, while in the Ural Mts. they are unidirectional and with small amplitude.
Słowa kluczowe (w języku angielskim): river pattern, river channel changes, fluvial processes.
Prace Geograficzne, 2006, z. 116, s. 111-118.
Instytut Geografii i Gospodarki Przestrzennej UJ
Patterns in the development of horizontal river channel transformations in the Republic of Udmurtiya, Russian Federation
The impact of active debris-flows from tributary valleys on channel development in mountain rivers (example of the River Baksan)
© IGiGP UJ "2022"