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
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)
Summary: The impact of valley debris-flows (siela2 in Russian) on the main channel development and fluvial processes involves a direct influence on the channel itself and an indirect influence of a modified pattern of water and bedload discharge. Taking into account the mutual influences of the main river and the valley debris-flows four main types of debris-flow impact nodes (DIN) were identified in the Baksan valley. The most evident impact of valley debris flows on the main river channel and its longitudinal profile can be seen in the type one impact zone. It characteristically features torrential cones and evident nick-points of the longitudinal profile. Three types of reaches can be identified in the main river channel in this zone: headwater reach, direct impact reach and a reach with active transformation of the supplied debris. This DIN tends to evolve at the confluences with tributaries with highly frequent debris-flows containing large volumes of material.
Słowa kluczowe (w języku angielskim): mountain river, channel, longitudinal profile, torrential cone, valley debris-flows, debris-flow impact nodes.
Prace Geograficzne, 2006, z. 116, s. 133-142.
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Ostatnia aktualizacja: 2017-12-08