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The Effects of Rising Sea Levels on the United States Coast of the Gulf of Mexico

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1. Introduction As it stands today the U.S. coast of the Gulf of Mexico is losing more and more land; the amount of land lost each year may seem relatively small to the average person, but to scientists who understand the unprecedented rate at which this is happening, there is reason to be alarmed. On the U.S. coast of the Gulf of Mexico there are more reasons for the rising sea level than simply global warming and melting ice sheets or ice caps. In the Mississippi delta, for example, the oil industry is taking so much fluid (oil) out of the ground that the land is sinking and compacting further. There is also a decrease in the amount of sediment reaching the delta due to many man-made structures, such as levees, drudging, dikes, and …show more content…

Rising sea level can be caused by a variety of factors and can have an effect or influence even more. Future changes in sea level may impact human populations around the world and many other aspects of life on Earth more than many initially thought. The U.S. coast of the Gulf of Mexico is on track to be one of the most impacted by further sea level rise and the outcome could be detrimental to the entire coastline. 2. Body

2.1 Past fluctuations in sea level: similar or different from today? Over the past several million years sea level has fluctuated considerably higher and lower than present levels. With these fluctuations the shoreline has shifted inland and further out, onto the continental shelf, than the present shorelines. The Northern Gulf of Mexico has followed the general path of global sea level during recent geologic time including the time since the last glacial maximum. During the last glacial maximum, 20,000 years ago, the sea level dropped approximately 100m below the present level and the shoreline extended 100km onto the shelf in some locations (Donoghue, 2011). Since the last glacial maximum the U.S. coast of the Gulf of Mexico has seen a rise in sea level at a rate exceeding those seen at any other time. The rate of overall sea level rise since the last glacial maximum is 6mm a year with some periods of rise in excess of 40mm a year. The rate has slowed and stabilized over the last 6,000 years and this has allowed ecosystems and

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