Analysis of the contemporary geomorphology, vegetation and in-channel wood within the relatively pristine Thurra River in southeastern Australia provides insight into river behaviour prior to European disturbance. This sand-bed river has an extremely low channel capacity with a pronounced pool-riffle morphology. Lateral migration rates are low (11-24 mm a⁻¹), as are floodplain aggradation rates (average = 0·27 mm a⁻¹). Sedimentological evidence is used to place contemporary channel dynamics within a 16 ka evolutionary framework. The floodplain has continuously aggraded over this interval, despite a number of avulsions and numerous meander cutoffs. Avulsions occur on a timeframe of once in 5 ka or more, while cutoffs occur around once in 1 k...
Historically, perceived increases in erosion and flooding levels have been attributed to in-stream w...
Clearance of riparian vegetation and removal of woody debris are perhaps the most pervasive of all f...
Anastomosing river plains of the Channel Country, central Australia, have aggraded slowly over the p...
Numerous case studies have demonstrated that alluvial and semi-alluvial rivers in SE Australia have ...
Water and sediment flux interactions are examined in Magela Creek, an alluvial (anabranching) sand b...
A riparian seed bank is a reserve of viable seeds and propagules in sediments of a river channel, ch...
Mediated equilibrium: The influence of riparian vegetation and wood on the long-term evolution and ...
Widden Brook in the Hunter Valley, Australia, was first settled by Europeans in 1831 and had widened...
Catastrophic channel changes on Wollombi Brook were initiated in June 1949 by a flood with a peak di...
A total of 436 logs were used to create 20 engineered log jams (ELJs) in a 1.1 km reach of the Willi...
Recent Australian research has quantified the role of large wood (wood of any origin and length with...
© 2017 Dr. Justin StoutMany anabranching rivers depend on the development and maintenance of avulsio...
The state of river channels and their riparian zones in terms of geomorphology and vegetation has a ...
The present morphology of a river is the outcome of past and present conditions. To understand a flu...
Dryland rivers are recognized for limited research and high uncertainties with respect to understand...
Historically, perceived increases in erosion and flooding levels have been attributed to in-stream w...
Clearance of riparian vegetation and removal of woody debris are perhaps the most pervasive of all f...
Anastomosing river plains of the Channel Country, central Australia, have aggraded slowly over the p...
Numerous case studies have demonstrated that alluvial and semi-alluvial rivers in SE Australia have ...
Water and sediment flux interactions are examined in Magela Creek, an alluvial (anabranching) sand b...
A riparian seed bank is a reserve of viable seeds and propagules in sediments of a river channel, ch...
Mediated equilibrium: The influence of riparian vegetation and wood on the long-term evolution and ...
Widden Brook in the Hunter Valley, Australia, was first settled by Europeans in 1831 and had widened...
Catastrophic channel changes on Wollombi Brook were initiated in June 1949 by a flood with a peak di...
A total of 436 logs were used to create 20 engineered log jams (ELJs) in a 1.1 km reach of the Willi...
Recent Australian research has quantified the role of large wood (wood of any origin and length with...
© 2017 Dr. Justin StoutMany anabranching rivers depend on the development and maintenance of avulsio...
The state of river channels and their riparian zones in terms of geomorphology and vegetation has a ...
The present morphology of a river is the outcome of past and present conditions. To understand a flu...
Dryland rivers are recognized for limited research and high uncertainties with respect to understand...
Historically, perceived increases in erosion and flooding levels have been attributed to in-stream w...
Clearance of riparian vegetation and removal of woody debris are perhaps the most pervasive of all f...
Anastomosing river plains of the Channel Country, central Australia, have aggraded slowly over the p...