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5.6: Submarine Canyons

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    Submarine canyons are similar to river gorges carved in mountainous regions on land, however they tend to be both much larger and deeper. Characteristics of submarine canyons include:

    • They generally form perpendicular to coastline.
    • They are commonly associated with zones of weakness such as a fault or a drowned river valley (canyons flooded by sea level rise).
    • They start on continental shelf and cut into (erode) shelf and upper slope, commonly near the mouth of a bay or river.
    • They are carved by undersea erosion processes associated with turbidity currents. Turbidity currents transport sediment into deep ocean basins via submarine canyons.
    • Turbidity currents moving down submarine canyons eventually slow down and deposit sediments on the continental rise as deep-sea fans.

    Hudson Canyon
    Figure \(\PageIndex{1}\): Hudson Canyon offshore of New York City

    5.6: Submarine Canyons is shared under a not declared license and was authored, remixed, and/or curated by Miracosta Oceanography 101 (Miracosta)) via source content that was edited to conform to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.