Sediment budget of a cuspate shoreline and its influence on spit development—Lagoa dos Patos, Brazil

2022 ◽  
Vol 42 (1) ◽  
Author(s):  
Inaiê Malheiros Miranda ◽  
Elírio Ernestino Toldo ◽  
Antonio Henrique da Fontoura Klein ◽  
Guilherme Vieira da Silva ◽  
Darrell Strauss
Keyword(s):  
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

1996 ◽  
Vol 33 (5) ◽  
pp. 664-675 ◽  
Author(s):  
Scott R. Dallimore ◽  
Stephen A. Wolfe ◽  
Steven M. Solomon

A long-term sediment budget (1947−1985) for northern Richards Island shows that, when ground ice and offshore erosion are accounted for, there is a near balance between headland erosion and coastal deposition. Excess ice constitutes about 20% of the total volume of eroded material from the headlands, with massive ground ice contributing nearly 9% and segregated ice lenses and ice wedges making up the remainder. Coastal response to major storms in 1987 and 1993 suggests that erosion is episodic, with short periods of intense disruption followed by readjustment of cliff profiles. Processes characteristic of this environment include mechanical erosion of ice-bonded sediments creating unstable erosional niches, mechanical failure of niches along ice-wedge planes, and longer term thermal erosion of ice-bonded sediments. Where ice contents are high, localized thaw slumps initiated by coastal erosion may retreat at rates substantially higher than those observed at other sections of the coast. Cliff-top retreat rates may be out of phase with storm-event chronology.


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