The sediment budget of a highly dynamic mesoscale catchment: The River Isábena

Geomorphology ◽  
2012 ◽  
Vol 138 (1) ◽  
pp. 15-28 ◽  
Author(s):  
J.A. López-Tarazón ◽  
R.J. Batalla ◽  
D. Vericat ◽  
T. Francke
Geomorphology ◽  
2009 ◽  
Vol 109 (3-4) ◽  
pp. 210-221 ◽  
Author(s):  
J.A. López-Tarazón ◽  
R.J. Batalla ◽  
D. Vericat ◽  
T. Francke

2002 ◽  
Vol 81 (2) ◽  
pp. 211-215 ◽  
Author(s):  
R.T. Van Balen ◽  
R.F. Houtgast ◽  
F.M. Van der Wateren ◽  
J. Vandenberghe

AbstractUsing marine planation surfaces, fluvial terraces and a digital terrain model, the amount of eroded rock volume versus time for the Meuse catchment has been computed. A comparison of the amount of eroded volume with the volume of sediment preserved in the Roer Valley Rift System shows that 12% of the eroded volume is trapped in this rift. The neotectonic uplift evolution of the Ardennes is inferred from the incision history of the Meuse River system and compared to the subsidence characteristics of the Roer Valley Rift System. Both areas are characterized by an early Middle Pleistocene uplift event.


2012 ◽  
Vol 60 ◽  
pp. 14-29 ◽  
Author(s):  
Andrew Morang ◽  
Jeffrey P. Waters ◽  
Syed M. Khalil

2009 ◽  
Vol 23 (22) ◽  
pp. 3230-3235 ◽  
Author(s):  
Mario L. Amsler ◽  
Edmundo C. Drago

2008 ◽  
Vol 33 (5) ◽  
pp. 695-711 ◽  
Author(s):  
Jan Nyssen ◽  
Jean Poesen ◽  
Jan Moeyersons ◽  
Mitiku Haile ◽  
Jozef Deckers

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