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5.6: The Littoral Cell

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    31620
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    The sand on a beach on any given day may be thought of as a reservoir, a place where something is stored. The size of this reservoir represents a balance between sources—processes that add to the reservoir—and sinks—processes that remove from the reservoir. Applying this idea, we may think of a beach as a reservoir of sand. Rivers and coastal erosion that bring sediments to the beach act as sources. Submarine canyons that remove sand from the beach are a sink. We can use this model to understand why some beaches grow in size, why some shrink, and why others seem to maintain a balance of sand over time.

    The watershed-beach-submarine canyon system—the path of sand from the mountains to the seafloor—form a system known as a littoral cell (or coastal cell). The concept of a littoral cell originated from a desire to understand why sand disappears on some beaches. The littoral cell embodies the sources, transport path, and sinks that determine the size of a beach.

    The balance between sources and sinks in a littoral cell can be modeled in terms of a beach sand budget (e.g., Bowen and Inman 1966). This accounting of the sources and sinks helps beach managers evaluate strategies for maintaining an adequate reservoir of sand. We won’t go into the mathematics here, but understanding the basic idea that sources add sand to the beach and sinks take sand away will help you appreciate efforts to understand human impacts on beaches and efforts to preserve these critically important habitats.


    This page titled 5.6: The Littoral Cell is shared under a CC BY 4.0 license and was authored, remixed, and/or curated by W. Sean Chamberlin, Nicki Shaw, and Martha Rich (Blue Planet Publishing) via source content that was edited to the style and standards of the LibreTexts platform.