The problem of how turbidity currents erode their beds is important for understanding
how submarine canyons develop, how they maintain continuity in tectonically active margins
to ensure sediment bypass, and for knowing how knickpoints (reaches of anomalously steep
gradient) record tectonic information. The problem is potentially more complex than fluvial
erosion because flow vigor is also varied by the flow entraining ambient water and
incorporating or depositing suspended load, which can significantly affect its excess density.
However, in canyon sections where the total sedimentary mass passing through the canyon
has been much larger than the locally excavated mass, the solid loads of eroding currents
changed little during passage down-canyon. Canyon morphology can then potentially reveal
how gradient and other factors affect erosion rate. Simple bed erosion models are developed,
analogous to the detachment- and transport-limited erosion models of fluvial
geomorphology, which predict that the channel topography should advect or diffuse (smooth
out), respectively. Datasets from continental slopes off Alaska, New Jersey, Oregon, Chile,
the Barbados accretionary prism and published maps from other areas are examined for these
tendencies. Although knickpoints may arise from spatially varied resistance to erosion, some
of those described here lie upstream of faults or anticlines and within uniform turbidites,
implying that they can advect upstream. A forward numerical model is developed for
knickpoints in the southern Barbados accretionary prism, which appear to have been created
in a simple manner by the front-most thrusts. If the erosion rules are applied continuously,
the channel profiles are well represented with both advective and diffusive components. If a
boundary condition of non-deposition/erosion is imposed on the base of the knickpoint slope
(representing scour associated with a hydraulic jump, for example), the upstream profiles can
be reproduced by solely diffusion. In these channels, the threshold stress for transport or
erosion was probably small relative to stress imposed by the currents because modeling
shows that a threshold sharpens the knickpoint lip rather than rounds it. Over the other,
mostly smaller, knickpoints studied, however, the lip varies from sharp to rounded. This varied morphology could arise from a number of influences: effects of flow acceleration,
differing threshold stress, differing sediment flux affecting flow power or depth-varying
substrate resistance to erosion. Despite the diversity of forms, up-stream migrations imply
that erosion can be enhanced where flow is more vigorous on steep gradients, implying that
the body rather than the head of turbidity currents is responsible for erosion in those cases. It
is speculated how bed failure, quarrying and abrasive scour leads to knickpoint evolution in
submarine channels that is analogous to that in fluvial channels but also likely differences.
Mitchell, NC, "The morphologies of knickpoints in submarine canyons", Geol. Soc. Am. Bull., 118, 589-605, 2006.