Interpretation of sedimentation data measured in a former tidal channel Lake Volkerak

1992 ◽  
pp. 107-118
Author(s):  
G. H. Tamminga
Keyword(s):  
Tidal Channel

scholarly journals Geomorphology of Scour Holes at Tidal Channel Confluences

2018 ◽  
Vol 123 (6) ◽  
pp. 1386-1406 ◽  
Author(s):  
Christian Ferrarin ◽  
Fantina Madricardo ◽  
Federica Rizzetto ◽  
William Mc Kiver ◽  
Debora Bellafiore ◽  
...  
Keyword(s):  
Tidal Channel ◽  
Scour Holes

scholarly journals Multi-scale temporal patterns in fish presence in a high-velocity tidal channel

PLoS ONE ◽  
2017 ◽  
Vol 12 (5) ◽  
pp. e0176405 ◽  
Author(s):  
Haley A. Viehman ◽  
Gayle Barbin Zydlewski
Keyword(s):  
High Velocity ◽  
Temporal Patterns ◽  
Tidal Channel ◽  
Multi Scale

Bio-geomorphic effects on tidal channel evolution: impact of vegetation establishment and tidal prism change

2012 ◽  
Vol 38 (2) ◽  
pp. 122-132 ◽  
Author(s):  
Wouter Vandenbruwaene ◽  
Tjeerd J. Bouma ◽  
Patrick Meire ◽  
Stijn Temmerman
Keyword(s):  
Tidal Channel ◽  
Tidal Prism ◽  
Channel Evolution ◽  
Vegetation Establishment

Sedimentary signals of fluvial discharge variability under tide and wave influence: Miocene examples in NW Borneo

2021 ◽  
Author(s):  
Daniel Collins ◽  
Howard Johnson
Keyword(s):  
River Discharge ◽  
Tidal Channel ◽  
Flood Wave ◽  
Wave Processes ◽  
Stratigraphic Architecture ◽  
Modern Analogue ◽  
River Flood ◽  
Sedimentary Dynamics ◽  
Tidal Variations ◽  
Tidal Processes

<p>The interaction of river and marine processes in the fluvial to marine transition zone (FMTZ) fundamentally impacts sedimentary dynamics and deposition. Heterolithics are important facies within ancient and modern FMTZs but the preserved signal of river flood, wave and tidal variations in heterolithics remains uncertain. This study integrates facies and ichnofacies characteristics of heterolithics in the Lambir Formation (Baram Delta Province, NW Borneo), with information of larger-scale stratigraphic architecture and modern analogue information, to interpret the preserved record of river flood deposits under the influence of tides and waves in an ancient FMTZ. Within the FMTZ of distributary channels, interpreted proximal–distal sedimentological and stratigraphic trends suggest: (1) a proximal fluvial-dominated, tide-influenced subzone; (2) a distal fluvial- to wave-dominated subzone; and (3) a conspicuously absent tide-dominated subzone. During coupled storm and river floods, fluvial processes dominated the FMTZ along major and minor distributary channels and channel mouths, causing significant overprinting of preceding interflood deposits and deposition of thicker, sandier event beds. Intervening interflood deposits are muddier, with increased bioturbation, and may variably preserve sedimentary indicators of tide and wave processes. Despite interpreted fluvial–tidal channel units and mangrove influence implying tidal processes, there is a paucity of unequivocal tidal indicators (e.g. cyclical heterolithic layering). This suggests that process preservation in the FMTZ preserved in the Lambir Formation primarily records episodic (flashy) river discharge, river flood and storm overprinting of tidal processes, and possible backwater dynamics. </p>

Seafloor morphology and habitats of tidal channels in the Venice Lagoon, Italy tidal channel habitats

2020 ◽  
pp. 187-198
Author(s):  
Fantina Madricardo ◽  
Giacomo Montereale-Gavazzi ◽  
Marco Sigovini ◽  
Aleksandra Kruss ◽  
Carlotta Toso ◽  
...  
Keyword(s):  
Venice Lagoon ◽  
Tidal Channel ◽  
Tidal Channels ◽  
Seafloor Morphology

On luminescence bleaching of tidal channel sediments

2015 ◽  
Vol 115 (1) ◽  
pp. 57-65 ◽  
Author(s):  
Mikkel Fruergaard ◽  
Morten Pejrup ◽  
Andrew S. Murray ◽  
Thorbjørn J. Andersen
Keyword(s):  
Tidal Channel
Sign in / Sign up

Export Citation Format

Share Document