Mountain headwater streams are still somewhat on the boundary of interest regarding possible human impact on their morphology or geomorphic processes, which may be caused by our perception of mountains as islands of relatively preserved natural conditions. This paper summarizes the past and present human pressure on the headwater streams that drain the highest mountain ranges of the Outer Western Carpathians in Czechia. Anthropogenic pressure began in this region in the 16th century during a colonization of the mountains and continued by timber harvesting, timber floating, and construction of torrent control works until present. Each of these interventions produced a morphological response of the channels in relation to altered sediment or ...
In the northern slope of the Carpathian Mountains and in their foreland, river and stream channels h...
Wallachian (shepherd) colonisation of the upper parts of Carpathians, the second largest mountain ra...
Floods represent a common process in Tatra Mountain streams and may cause flood risk in the valleys ...
Comprehensive field survey of the physiographic context and channel morphology is a key to distingui...
In the northern slope of the Carpathian Mountains and in their foreland, river and stream channels h...
The hydromorphological conditions of watercourses depend on numerous natural and anthropogenic facto...
The Czarny Dunajec is a typical river originating in high mountains (the Western Tatras). Over the e...
This paper presents an analysis of both the contemporary and historic development of the geomorphic ...
Long stretches of Carpathian river channels have been engineered, which has had an impact on their m...
W opracowaniu przedstawiono stan badań dotyczących lejów źródłowych. Zwrócono szczególną uwagę na od...
In the last centuries, gravel-bed rivers in developed countries have undergone rapid changes in chan...
The formation processes of small valleys and long-term anthropogenic impact on its sedimentary archi...
Human modifications and related pressure on watercourses of its ecosystem became greatly discussed p...
Streams of the Polish Carpathians are characterized by a high gradient as well as a great changeabil...
Floods are considered to be a crucial agent influencing the formation of the floodplain. The knowled...
In the northern slope of the Carpathian Mountains and in their foreland, river and stream channels h...
Wallachian (shepherd) colonisation of the upper parts of Carpathians, the second largest mountain ra...
Floods represent a common process in Tatra Mountain streams and may cause flood risk in the valleys ...
Comprehensive field survey of the physiographic context and channel morphology is a key to distingui...
In the northern slope of the Carpathian Mountains and in their foreland, river and stream channels h...
The hydromorphological conditions of watercourses depend on numerous natural and anthropogenic facto...
The Czarny Dunajec is a typical river originating in high mountains (the Western Tatras). Over the e...
This paper presents an analysis of both the contemporary and historic development of the geomorphic ...
Long stretches of Carpathian river channels have been engineered, which has had an impact on their m...
W opracowaniu przedstawiono stan badań dotyczących lejów źródłowych. Zwrócono szczególną uwagę na od...
In the last centuries, gravel-bed rivers in developed countries have undergone rapid changes in chan...
The formation processes of small valleys and long-term anthropogenic impact on its sedimentary archi...
Human modifications and related pressure on watercourses of its ecosystem became greatly discussed p...
Streams of the Polish Carpathians are characterized by a high gradient as well as a great changeabil...
Floods are considered to be a crucial agent influencing the formation of the floodplain. The knowled...
In the northern slope of the Carpathian Mountains and in their foreland, river and stream channels h...
Wallachian (shepherd) colonisation of the upper parts of Carpathians, the second largest mountain ra...
Floods represent a common process in Tatra Mountain streams and may cause flood risk in the valleys ...