Abstract
On the continental shelves off large deltas, rapid progradation and deposition result in highly underconsolidated marine sediments. These deposits, which are often also rich in interstitial methane gas, can be subject to widespread and active mass movement downslope. For example, the submarine slopes of the Mississippi River delta are affected by a variety of sediment instability processes. Geologic and geophysical surveys using side-scan sonar, subbottom profilers, and precision depth recorders have been completed for the entire subaqueous delta. Survey lines were spaced at 240-m intervals, and water depths ranged from 5 m to 20 m. Bottom morphology, including sediment deformations indicative of instability, has been mapped at a scale of 1:12,000, and large-area, scale-corrected sonar mosaics have been constructed. The features identified include collapse depressions, bottleneck slides, shallow rotational slides, mudflow gullies, overlapping mudflow lobes, and a wide variety of faults. The slides and mudflows are extremely active, and movement rates of several hundred metres per year have been recorded. Damage to offshore oil and gas pipelines and platforms has occurred. Also, the concept of slow, continuous deltaic progradation must be modified to include the effects of these processes. For example, on the shelf, normal settling of suspended clays averages only a few millimetres per year, whereas at the front of the delta slope more than 30 m of sediment has been deposited by mudflows and slides since 1875.
These deltaic processes are the result of complex temporal and spatial combinations of different factors, including the generation of excess pore pressures by rapid sedimentation, methane gas within the sediments, wave-induced stresses, and localized slope oversteepening. These conditions are not unique to the Mississippi Delta, and indeed similar processes, which affect geologic deposition models and provide design constraints for offshore engineering, appear to be common in many deltaic environments.
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© 1982 Plenum Press, New York
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Prior, D.B., Coleman, J.M. (1982). Active Slides and Flows in Underconsolidated Marine Sediments on the Slopes of the Mississippi Delta. In: Saxov, S., Nieuwenhuis, J.K. (eds) Marine Slides and Other Mass Movements. NATO Conference Series, vol 6. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-3362-3_3
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DOI: https://doi.org/10.1007/978-1-4613-3362-3_3
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