Unit bars are relatively large bedforms that develop in rivers over a wide range of climatic regimes. Unit bars formed within the highly-variable discharge Burdekin River in Queensland, Australia, were examined over three field campaigns between 2015 and 2017. These bars had complex internal structures, dominated by co-sets of cross-stratified and planar-stratified sets. The cross-stratified sets tended to down-climb. The development of complex internal structures was primarily a result of three processes: (i) superimposed bedforms reworking the unit bar avalanche face; (ii) variable discharge triggering reactivation surfaces; and (iii) changes in bar growth direction induced by stage change. Internal structures varied along the length and ...
Distinguishing the deposits of mouth bars from delta distributary channels in the rock record may no...
Cross-stratified sandstones formed by dunes and unit bars is common in the rock record. Cross-bed ar...
This study investigates the occurrence and dynamics of single row alternate bars forming in a partic...
Unit-bar deposits are ubiquitous components of river-channel deposits and strongly influence their h...
Discharge event frequency, magnitude and duration all control river channel morphology and sedimenta...
This experimental investigation examines the processes that control the grain-size sorting and geome...
A hierarchical typology for the channels and bars within aggradational wandering gravel-bed rivers i...
Extant, planform-based facies models for alluvial deposits are not fully fit for purpose, because th...
Alternate bars in rivers and streams develop as a result of differences in length scales involved in...
AbstractUnderstanding of morphodynamic processes associated with large‐scale floods has recently imp...
Bars are key morphological units in river systems, fashioning the sediment regime and bedload transp...
Fluvial strata dominated internally by sedimentary structures of interpreted upper flow regime origi...
© 2017 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd. Bifu...
We illustrate the potential for using physics-based modeling to link alluvial stratigraphy to large ...
Sedimentation in a fluvial system leads to the formation of bars with varied morphology, bedform fea...
Distinguishing the deposits of mouth bars from delta distributary channels in the rock record may no...
Cross-stratified sandstones formed by dunes and unit bars is common in the rock record. Cross-bed ar...
This study investigates the occurrence and dynamics of single row alternate bars forming in a partic...
Unit-bar deposits are ubiquitous components of river-channel deposits and strongly influence their h...
Discharge event frequency, magnitude and duration all control river channel morphology and sedimenta...
This experimental investigation examines the processes that control the grain-size sorting and geome...
A hierarchical typology for the channels and bars within aggradational wandering gravel-bed rivers i...
Extant, planform-based facies models for alluvial deposits are not fully fit for purpose, because th...
Alternate bars in rivers and streams develop as a result of differences in length scales involved in...
AbstractUnderstanding of morphodynamic processes associated with large‐scale floods has recently imp...
Bars are key morphological units in river systems, fashioning the sediment regime and bedload transp...
Fluvial strata dominated internally by sedimentary structures of interpreted upper flow regime origi...
© 2017 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd. Bifu...
We illustrate the potential for using physics-based modeling to link alluvial stratigraphy to large ...
Sedimentation in a fluvial system leads to the formation of bars with varied morphology, bedform fea...
Distinguishing the deposits of mouth bars from delta distributary channels in the rock record may no...
Cross-stratified sandstones formed by dunes and unit bars is common in the rock record. Cross-bed ar...
This study investigates the occurrence and dynamics of single row alternate bars forming in a partic...