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Wave –Coast Interactions Wave patterns due to coastal interference. Diffracted Waves. Waves spread out , decreasing in height and energy. Radiating Waves. Waves move outward in concentric rings from the generating source. Reflected Waves. Waves that bounce off an object.
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Wave –Coast InteractionsWave patterns due to coastal interference
Diffracted Waves • Waves spread out, • decreasing in height • and energy
Radiating Waves Waves move outward in concentric rings from the generating source
Reflected Waves Waves that bounce off an object
Refracted Waves Waves bend around an obstacle, changing the direction of the wave
Converging Waves Waves that come together at a certain point, increasing the wave height and strength
Rip Currents Currents that flow away from the shore, toward the sea. Usually occurs when longshore currents flow toward each other, meet, and then flow out to sea. Strong at the point where the currents meet, but weakens as it flows out to sea
Eddy A circular motion of water on the surface
LongshoreCurents • Currents that flow parallel to the beach along the shoreline
Sand Transport • Movement of sand by waves and currents • Results in erosion (loss) and accretion (build-up) of beach • Movement results in sorting by size and density, resulting in the following beach formations
Sand Dunes Mounds of loose, windblown sand
Sandbar • Offshore, small sediment • accretion, usually submerged
Jetties • Protect entrances to waterways