Morphometric analysis of plunge pools and sediment wave fields along western Great Bahama Bank

• Published in: Marine geology Vol. 397; pp. 15 - 28
• Main Authors: Schnyder, Jara S.D., Eberli, Gregor P., Betzler, Christian, Wunsch, Marco, Lindhorst, Sebastian, Schiebel, Linda, Mulder, Thierry, Ducassou, Emmanuelle
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.03.2018
• Subjects: Carbonate slope; Cyclic steps; Density current; Great Bahama Bank; Multibeam bathymetry; Plunge pool; Sediment waves; Slope morphology; Supercritical flow conditions; Waveform; Density current; Waveform; Sediment waves; Great Bahama Bank; Cyclic steps; Carbonate slope; Plunge pool; Supercritical flow conditions; Slope morphology; Multibeam bathymetry
• ISSN: 0025-3227; 1872-6151
• DOI: 10.1016/j.margeo.2017.11.020

A systematic assessment of morphometric parameters of over 200 plunge pools along the steep escarpment base of western Great Bahama Bank and ~2000km2 of sediment wave fields of upslope migrating cyclic steps documents the importance of cascading density currents for sedimentation on the slope. The abrupt downslope termination of the Holocene mud wedge with the cyclic steps shows that strike parallel bottom currents interacting with the off-bank currents are responsible for slope sediment distribution. The plunge pools and sediment waves were generated by density-cascading and both are related to a hydraulic jump caused by two gradient changes along the slope profile. The bedforms highlight both the erosional and depositional nature of this current regime, which is controlled by slope gradient and the directional confinement by either grooves on the steep escarpment or gullies on the middle to lower slope. The >20m deep plunge pools are ellipsoidal, with an average width of 211m and length of 283m, but variations between 80–360m and 100–650m for width and length occur. They are caused by an average gradient break of 16° on the cemented upper slope. Gradient breaks of as low as 2° are reported to be sufficient to scour a plunge pool like the ones in the study area, but higher gradient breaks between 10 and 20° are quite common for consistent plunge pool development. A second gradient break further down slope changes flow conditions for the generation of cyclic steps, with asymmetric waveforms of 4m high (average) in large wave fields in the entire the study area. Orientation is mainly orthogonal to the main slope direction but wave lengths and sinuosity vary, depending on the morphologic location of the wave field. The comparison with sediment wave fields with similar geometries or in similar environments shows that flow reconstruction based on the wave height and wave length alone along with a characterization of sediment grain size, however, yields non-unique results and is site specific. •Sediment wave fields and plunge pools are the result of cascading density currents interacting with local slope geometry.•Grooves in the steep escarpment influence the cascading density currents by confining and channelizing the flow.•Bedforms and grain size distribution highlight erosional and depositional nature of this current regime.