OceanWorld |
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WAVES and THEIR AFFAIRS with COASTLINES The coast of all continents bear the marks of the sea. Some coastlines, like California's are narrow and rugged. Others, like the Atlantic coastal plain, rise gradually for hundreds of kilometers inland. Breaking waves shape and form our coastlines. Waves can deposit (deposition) and carry away (erosion) sediment. As waves batter against the coast, they constantly erode and grind away the shore. Rocks and cliffs that are undercut by wave action fall into the sea where waves weather them into sand. Sometimes the eroded material is carried seaward where it is deposited--sometimes forming sand bars. The shape of the coastline is determined by the original materials (i.e. rock types) and their resistance to wave erosion. How quickly erosion along the shore takes place depends on several factors one of which is the amount of energy released by the waves as they approach the coast or shore. Not all waves expend their energy on the shore. They may break farther seaward on sand bars or reefs. We've only touched the surface of the ocean (waves). You may want to expend (spend) more energy and surf the wave issue further. Some suggested topics for future investigation are: Types of waves (breaker, plunger, spiller, etc.), Kelvin and Rossby waves, types of coastlines and how they are formed, and human interactions that attempt to control erosion of coasts. Questions that come to mind are:
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