During the 1970s, the Palancia River was intensively affected by gravel mining instream. This activity completely destroyed the fluvial forms, devastating the original wandering pattern. At the end of the 1980s, gravel mining ceased and the river started a process of recovery, only altered by several clearing operations. The aim of this work is to describe these processes of change, analyzing the river's morphosedimentary conditions through a GIS analysis of aerial photographs previous to, simultaneous with, and subsequent to the intense gravel mining activity. Results explain the current difficulties of some ephemeral rivers to recover their original forms, because of the sediment and water deficit conditions, the critical role of channel ...
The alteration of sediment transport regime represents one of the key factors controlling the respon...
The lower Gállego River has been strongly degraded since the 1960s due to human activity (gravel min...
In ephemeral rivers, channel morphology represents a snapshot at the end of a succession of geomorph...
[EN] During the 1970s, the Palancia River was intensively affected by gravel mining instream. This a...
Gravel mining has been a widespread activity in ephemeral rivers worldwide whose long-lasting hydrog...
An analysis of morphological changes during the last six decades is presented for a 16.5-km reach of...
Many gravel bed rivers in the European Alpine area suffered different ranges and types of human pres...
This research focuses on analyzing the multiple causes of riverbed degradation along the lower reach...
Historical information was used to study river degradation in a case study in NE Spain. The accumula...
Many gravel bed rivers in the European Alpine area suffered different ranges and types of human pres...
This paper describes changes in bed morpho‐dynamics and topography in the River Ehen, a regulated ri...
[EN] In October of 2000, the Palància River underwent a major flood, which substantially modified t...
The aim of this paper is to explore possibilities and limitations of restoring physical processes in...
This paper examines the effects of gravel mining on the suspended sediment transport in the Upper Ri...
In ephemeral rivers, channel morphology represents a snapshot at the end of a succession of geomorph...
The alteration of sediment transport regime represents one of the key factors controlling the respon...
The lower Gállego River has been strongly degraded since the 1960s due to human activity (gravel min...
In ephemeral rivers, channel morphology represents a snapshot at the end of a succession of geomorph...
[EN] During the 1970s, the Palancia River was intensively affected by gravel mining instream. This a...
Gravel mining has been a widespread activity in ephemeral rivers worldwide whose long-lasting hydrog...
An analysis of morphological changes during the last six decades is presented for a 16.5-km reach of...
Many gravel bed rivers in the European Alpine area suffered different ranges and types of human pres...
This research focuses on analyzing the multiple causes of riverbed degradation along the lower reach...
Historical information was used to study river degradation in a case study in NE Spain. The accumula...
Many gravel bed rivers in the European Alpine area suffered different ranges and types of human pres...
This paper describes changes in bed morpho‐dynamics and topography in the River Ehen, a regulated ri...
[EN] In October of 2000, the Palància River underwent a major flood, which substantially modified t...
The aim of this paper is to explore possibilities and limitations of restoring physical processes in...
This paper examines the effects of gravel mining on the suspended sediment transport in the Upper Ri...
In ephemeral rivers, channel morphology represents a snapshot at the end of a succession of geomorph...
The alteration of sediment transport regime represents one of the key factors controlling the respon...
The lower Gállego River has been strongly degraded since the 1960s due to human activity (gravel min...
In ephemeral rivers, channel morphology represents a snapshot at the end of a succession of geomorph...