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5.1: What Is a Beach?

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    31615
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    The term beach commonly refers to the loose bits and fragments of material along the shore of a body of water, including lakes, rivers, and the world ocean. These bits and fragments consist mostly of sediments, solid particles of various sizes fragmented from rocks. While we think of beaches as mostly sand, they may include any of the six major size classes of sediments as defined in a geological classification system known as the Udden-Wentworth scale. From smallest to largest, they include clay, silt, sand, pebbles, cobbles, and boulders (Udden 1914; Wentworth 1922). Many beaches exhibit the full range of sediment sizes, from clay to boulders.

    Sediments also originate from biological and chemical processes. Fragments of shells, corals, and even calcified algae can be found on beaches. Sanibel Island on the west coast of Florida features beaches made almost entirely of intact or broken fragments of shells. Bahamian beaches accumulate ooids, light-colored ovals of calcium carbonate that resemble the hard mint candies known as Tic Tacs. Ooids originate from the precipitation of solids in supersaturated seawater.

    Beaches may host a wide variety of other materials, too—natural and manmade. Beaches in the state of Washington are often covered in driftwood and logs, castaways from the logging industry. The Skeleton Coast on the northern coast of Namibia accumulates the bones of whales, seals, and shipwrecks. And as you well know, debris from humans—especially plastics—can be found on every beach in the world, including those in Antarctica.


    This page titled 5.1: What Is a Beach? 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.