Coastal Erosion Term Papers

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Coastal erosion is an ecological hazard that has been occurring for centuries however rising sea levels and increasingly erratic weather patterns have the potential to advance the danger and destruction to much greater levels.  While the tumultuous wave action created by huge storms such as hurricanes is the most contributive to coastal erosion, the normal but repetitive wave action against the shoreline is just as destructive over the long-term.

Even after recent decades of catastrophic storm systems that have contributed to shoreline erosion and the intensified efforts by the U.S. Army Corps of Engineers, there is still no entirely successful or long lasting method for securing nature’s shorelines.  This deficit presents major implications for increased research on developing mechanisms that will secure shorelines and ultimately their inhabitants.

Although coastal shorelines have many similarities they can also be very diverse depending on their geographic location.  Similarly, their predisposition to erosion is also dependent on location.  Shorelines can be divided into seven different categories including barrier islands, coastal wetlands, bluffs and cliffs, strand plain beaches, coral reef and bedrock, all of which manifest coastal erosion differently.

On the Atlantic and Gulf coastlines, which are made up largely of barrier islands, the beaches are eroding at average annual rates of  3 and 6 feet respectively.  The devastating erosion demonstrated by severe storm weather on the Atlantic Coast has been exhibited for more than a century along the 200 mile New York and New Jersey coastline.  The cliffs and bedrocks on the Pacific coast shorelines erode less per year however they are more susceptible to immediate erosion from dramatic weather events, which can destroy hundreds of feet of shoreline at one time

There have been a variety of solutions created in the attempt to assuage the erosion process on shorelines including trapping and pumping sand into eroded areas or areas faced with erosion as well as consolidating groups of barrier islands into single “sandboxes”.  While these measures have worked to temporarily protect property, they have been unable to prevent erosion from catastrophic weather events that increase the size and intensity of wave action.

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