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Photos by: Mitch Miller




            Longshore Drift
            Have you ever noticed that when you’re resting
            on a floatie or paddling in a kayak, that the water
            tends to push you in either direction along the
            shoreline? Well, this is the same force that transports
            sediment parallel to the beach . This process is called
            longshore drift, and it is a combination of currents,
            incoming wave direction, and sometimes wind .
            Once the sediment is picked up and suspended
            in the water, it can be moved along the shoreline
            for many kilometers! The shape of the shoreline,
            including human-made structures, determines
            where that sediment is ‘dropped off .’  Littoral drift
            is the movement of sediment along the shore by
            longshore drift . Longshore and littoral drift are
            critical to creating and maintaining our beaches .


            Waves
            Waves typically hit the shorelines at an angle
            (refracted) and that results in energy being directed
            along the coastline in the direction of the incoming
            wave . This energy, known as longshore current, is
            similar to longshore drift and also contributes to
            erosion, deposition and transport of sediment .
            Wave energy works in multiple ways to transport
            and redistribute sediment . As a wave approaches
            the shore it enters shallow water and the wave base   In high energy shores that experience lots of wave
            scours the bottom, creating turbulence and picking   exposure, sands can be deposited and washed
            up sediment . As the wave crests and crashes onto   away seasonally with storms . Steady supplies of
            the shore, the sediment is further disrupted and   sediments being delivered by longshore drift
            picked up into the water column . The uprush of   processes allow accretion into dunes which
            water that moves onto the beach is called swash    become stabilized with vegetation and offer
            — this hits the beach, then the water retreats   protection to the areas above the tidal zone .
            back over the sand and stones as the next wave   As sea levels change these buffers naturally
            approaches the shore .                          migrate and continue to protect our shores .

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