Deep Sea Research Part A. Oceanographic Research Papers
Baltimore Canyon as a modern conduit of sediment to the deep sea
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Cited by (183)
Consumer isoscapes reveal heterogeneous food webs in deep-sea submarine canyons and adjacent slopes
2024, Progress in OceanographyOn the occurrence of low concentration hyperpycnal river plumes in a small mountainous river-canyon system
2023, Continental Shelf ResearchCombining stratigraphic forward modeling and susceptibility mapping to investigate the origin and evolution of submarine canyons
2022, GeomorphologyCitation Excerpt :In addition, submarine canyons are initiated by mass movements and gravity flows. Hence, the morphology and evolution of submarine canyons could reveal the behaviors of these two dominant processes in deep-water settings (Gardner, 1989; Hui et al., 2019; Nelson et al., 2011; Normark et al., 2003; Qin et al., 2017). Due to the difficulty in directly measuring deep-water processes, especially in geological timescales, there still exists an unsettled debate between the upslope and downslope erosion models regarding submarine canyon evolution.
Turbidity Current
2022, Treatise on GeomorphologyPhysico-chemical factors regulating marine benthos structure and function
2022, Ecology and Biodiversity of BenthosDistributions of microplastics and larger anthropogenic debris in Norfolk Canyon, Baltimore Canyon, and the adjacent continental slope (Western North Atlantic Margin, U.S.A.)
2022, Marine Pollution BulletinCitation Excerpt :These currents often originate in or near the heads of submarine canyons and are known to exist in Norfolk Canyon (Boggs, 2006; CSA et al., 2017). Baltimore Canyon also channels turbidity currents and focuses internal tides to transport sediments to the deep sea (Gardner, 1989). Sediments entrained in such currents generally settle within canyons in a “fining up” sequence, where larger coarse grain sediments are first to be deposited.