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Cold-water coral ridges with waveform morphology are commonly observed in mound surfaces in the Northeast Atlantic Ocean and interpreted as sediment waves overgrown by corals. This work documents the first cold-water coral ridges that are waveform but lack sand dune cores. These coral ridges are situated at the base of the Miami Terrace in the Straits of Florida (depths of 630 to 870m). They are entirely...
Cold‐water coral mound morphology and development are thought to be controlled primarily by current regime. This study, however, reveals a general lack of correlation between prevailing bottom current direction and mound morphology (i.e. footprint shape and orientation), as well as current strength and mound size (i.e. footprint area and height). These findings are based on quantitative analyses of...
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