What is a long coast?

Drift drift is a natural process describing the current that often moves mostly parallel to the beach coast. Although this type of phenomenon has always happened, it is largely considered to be harassing because of the way in which the beach can change in some areas. Many of them refer to this drift as erosion because it moves sediment on the beach and can cause sand deficiency in some areas. Some strategies have been successfully used to stop the effects of a long coast drift, but some feel that these experiments were eventually at the expense of the environment.

The long coast drift begins when the waves hit the beach. Waves usually do not hit the coast straight, but at an angle. When reverse rinsing goes out, it takes some sand. The current that goes in the same way as the direction of the waves takes part of the suspended sand down the coast until the next wave lifts it and puts it back to the beach. The current rarely changes due to the predominant wind of Aznov, the sand usually never returns to its original locationof it.

The main problem with the long coast drift concerns the removal of sand from one place and storing it in another. Although such things help shape the natural and different coast of the beach, it can be uncomfortable for some property owners. Those who have as much as possible are resort owners who depend on people coming to enjoy a nice beach. If the drift takes too much sand, it can actually eat on permanent soil, causing a more serious form of erosion that could eventually endanger the structure.

To fight erosion is one of the most common practices to build a wall that extends from the coast to the ocean at an angle of 90 degrees in relation to the coast. This helps break the current and prevents drift. Some places can use waves built at sea to stop the waves, and aletato technique also breaks the waves before reaching the coast, which may be desirable in some places.

use of physicalThe barrier to stop the drift on the long coast also caused controversy. Some groups believe that practice does not allow the natural tide and the flow of the beach. Furthermore, as soon as the person stands upstream to keep the sand, it forces others down the border to take the same actions or are taken from them, but will never be replaced by other sand from upstream. This often leads to a long series of pier along the coast.

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