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5 disadvantages of soil erosion
5 disadvantages of soil erosion
Conclusion on the effect of soil erosion
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• Longshore drift occurs as the movement of particles going in and out of the ocean causes these particles to move up and down the coast and beach. This movement forms the coastline at Point Peron. At Point Peron the longshore drift is heading in a Southerly direction, causing the particles to move down the beach as shown in the photograph below. The waves are coming onto the beach carrying particles of sand and small sediments such as shell pieces, which are deposited onto the beach before the water recedes. Along the Mandurah coast going northwards, the seasonal movement of sand is stopped by the construction of groynes. This causes the sand to build up on one side of the groyne.
• Constructive waves carry the materials that are laid down on the beach. This process forms the beaches. As the waves come into shore at Point Peron the deposition of sand and small sediments are placed on the beach. Over time this creates a larger beach and smoother sand.
• Destructive waves are large waves that carry more materials that crash into the mainland rock. This type of wave forms bays and headlands. Over time the waves break down the mainland into an arch, which then breaks off into a stack, and then breaks down into a stump. Eventually there is nothing left there. This process happens over a very long period of time. Destructive waves are very powerful and strong waves. They also break down sediments that come into the shore line.
• Erosion is the wearing away of rock by water and wind. This process occurs at Point Peron as erosion forms rock formations, arches, stacks and stumps much like destructive waves. Erosion has also caused the sand dunes to form from the wind blowing the sand into large mounds. Over a ...
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...d area to prevent further environmental damage.
• The drains have been built to remove excess water from the streets and paths making them safer to drive and walk on.
• The jetty has been built for the residents to walk out on without actually getting wet. It is also built for the locals to park their boat.
• The bins have been built for the community to dispose of their waste properly, and stopping it from going into the environment.
• The sea wall has been built to stop erosion taking place on the mainland and to protect the hotels, businesses and residential housing.
• The harbour has been built for the locals to bring their boat into house which is on the canal.
• The park has been built for the residents and locals to have an open space to enjoy nature.
The cultural objects shown demonstrate the ways they enhance the way of life of the community.
However, if any action is taken to defend the coastline, if you hinder in nature's course of beach erosion, there will always be after effects resulting from unnatural intrusion. This proves that any sea defence could prove a problem especially with the land owned by Nation Trust. Nevertheless if you could prove to the owners of the land to the extent of which erosion is taken place and show them how much LSD is affecting the area, action may well become a better option.
Investigating the Geographical Processes that are Affecting the Physical and Built Coastal Environment There are three geographical processes that are affecting the physical and built coastal environment, they are; erosion, deposition, and transportation. Erosion is the group of natural processes, including weathering, dissolution, abrasion, corrosion, and transportation, by which material is worn away from the earth’s surface, this is mainly caused by wind, running water, and waves breaking on the coast. Deposition is the depositing something or the laying down of matter by a natural process. Transportation is when sand is moved along the coast by long shore drift. At North Cronulla beach erosion is evident.
To do so, various stages of protection work were carried out. The first of these was the main protection of the cliff face; the aim was to prevent any falling rock and also cliff retreat with the hope that this would affect the input sediment rate, slowing it down. An extremely important coastal work implemented at the cliff sites from Hastings eastwards towards Fairlight. It was important however, to implement such works on the cliffs, because of their composition or geology that being soft sandstone with a shingle base all along the coastline.
There are many different types of coasts that exist throughout the United States. The south shore of Long Island has a unique types of coast known as a barrier beach. Barrier beaches are long narrow land forms that are composed of sand and other lose sediments. These sediments are brought together by the actions of waves, currents and storm surges. Barrier beaches are subject to constant changes by the same forces. Sand is constantly eroded in one area an deposited in another. Barrier coasts are important for a number of reasons; they protect the mainland of Long Island from the open ocean and flooding during storms, for recreational use and the unique ecosystems which exist on barrier beaches.
Longshore drift is a process by which sediments are transported from one place to another. When this process occurs, beaches, spits and sandbars are accreted over time. If the process of longshore drift is altered by factors such as stronger winds and stronger currents, beach erosion begins at a faster rate and this may result in many serious problems. The main stakeholders of longshore drift are resort owners. They rely on people to visit their resorts and enjoy the beach. However, if longshore drift erodes too much sand, it can permanently deprive sand from the area, which can also threaten structures close to the shoreline.
Coastal Erosion and Defence in White Cliffs Country Introduction The shoreline is a dynamic system where stability is maintained despite the continued movement of waves, tides, wind and sediment. The present configuration of the shoreline is now controlled by the various coastal defences', which mankind has put in place over the last 100 - 200 years. These have stopped or slowed the transport of sediments and reduced the ability of the shoreline to respond to Natural forcing factors. Who is responsible for the coastline?
Galveston Island is a barrier island formed during the Holocene after a major glacial melt. Since that time, the island has changed in size and geographic location based on numerous factors including sediment availability and various hydrodynamic reasons. The island also suffers from erosion due to major storms, like hurricanes, as well as other natural disasters. Much effort has been put in place to reduce the amount of erosion and/or migration, including a seawall and jetties. These efforts are not 100% effective and while the island will continue to transform; with human intervention, we hope to mitigate this change to a minimum.
Out of all the natural disasters that we talk about in class, the most deadly would have to be a Tsunami. Compared to earthquakes, Tsunamis have cause more deaths since 1945. A Tsunami is likely to strike anywhere on the west coast, including Santa Cruz in California – United States – North America – 36:58:24N 122:02:09W. A Tsunami is a giant “wave” of water that is caused by a sudden shift in the sea floor. The wave is a result of the water attempting to regain its equilibrium, which is driven by gravity. The size of the wave is determined by how much the sea floor is moved vertically, and how quickly it shifts. A greater water depth helps as well. They can travel up to five hundred miles an hour and have wave heights of one hundred feet. Earthquakes are the leading cause of Tsunamis. People who live in California are well aware of earthquakes that are frequently caused by the San Andreas Fault. However, not many are aware of the results of earthquakes that occur out in the Pacific Ocean. Tsunamis have also been referred to in the past as seismic sea waves, but Earthquakes aren’t the only cause of this phenomenon. Landslides, nuclear explosions, volcanic eruptions, and extra terrestrial impacts also have great water displacement results.
All naturally occurring stone arches are formed by the selective erosion of rock, but the terms by which this can occur are massive. Among the most frequent types of formation are wave action and lava flow. During wave action, water crashes constantly upon the rock, effectively accelerating erosion while sediment carried by the water is extremely abrasive, removing bits of rock. When lava flow occurs, the outermost la...
The Sun’s radiation heats the upper atmosphere, sending the energy toward the earth’s surface and finally mixes with the planet’s counter-rotational currents, creating jetstream flows. The winds flow over the ocean’s surface creating friction that spawns chops, pushing up the seas forming perfect bands of open ocean swell. Pushed on by gravitational forces, the swells speed away from the winds that they came from, moving across the deeps until they feel the drag of the shallows near the coast. As the swells rise up out of themselves, they peak, curling into the liquid dreams that we surfers ride (Kampton 4).
Semaphore Beach is affected by many factors such as natural processes and human impacts including marine litter and the discharge of stormwater. Therefore, several plans have been employed to ensure that the coast is supported through the method of counteracting erosion. However in the future, many management strategies have been put into consideration as well as the environmental, economic and social impacts as well as the predicted consequences. These impacts include traffic related incidents, noises and air pollution and the disruption of wildlife and the erosion of dunes. A method that should be considered for future management of the beach is the use of a concave sea wall, although efficient, this structure would be quite costly. Without the use of coastal management, Semaphore Beach would be unsupported, therefore negatively being affected by a variety of
. Cape Hatteras Lighthouse is the 208-foot tall landmark was just hauled more than a quarter-mile back from its former perch, where it was threatened by the encroaching sea. Coastal erosion chewed away about 1,300 feet of beach, bringing the waves to within 150 feet of the 4,800-ton sentinel. When the light was erected in 1870, it stood about 1,500 feet back from the waves. The lighthouse, on the Outer Banks, North Carolina's long barrier beach, was built to warn ships from waters called "the graveyard of the Atlantic." Ironically, the move should serve as a warning about the growing problem of coastal erosion. Erosion is not just plaguing the Outer Banks. Coastal residents up and down the United States are worrying about undermined cliffs, disappearing beaches, and the occasional dwelling diving into the briny. Beaches are constantly moving, building up here and eroding there, in response to waves, winds, storms and relative sea level rise. Yet when commoners like you and me, and celebs like Steven Spielberg, build along the beach in places like Southampton, N. Y., we don't always consider erosion. After all, real-estate transactions are seldom closed during hurricanes or northeasters, which cause the most dramatic damage to beaches. Yet Southampton, like all the barrier beaches that protect land from the sea, is vulnerable to obliteration by the very factor that makes it so glamorous: the sea. And the problem is increasing because the sea is rising after centuries of relatively slow rise, and scientists anticipate that the rate of rise will continue to increase in the next century. Land, in many places, is also slowly sinking. The result is a loss of sand that places the occasional beachside home inconveniently near -- or in -- the water. Still, erosion cuts in two directions. Without the process of erosion, we would not have the beaches, dunes, barrier beaches, and the highly productive bays and estuaries that owe their very existence to the presence of barrier beaches. Erosion of glacial landforms provides most of the beach sand in Massachusetts. A popular destination The beach-erosion problem has many causes. Among them are: · The ubiquitous desire to live near the sea. · A historically rapid ri...
is being eroded by the sea so that cliffs, up to 20 metres high rise
Our world is getting to the point to where we will be surrounded by trash. There are hazards happening because of the excess trash, which could have been recycled. Although the government is not doing their best to make these hazards stop, surprisingly it is the non-governed organizations that are trying to make the difference. Proven studies and facts have been made about these issues, so people should take this into consideration and start recycling more. Recycling is a beneficial process that is not required globally like it should be because citizens are uneducated on the process and what it can do. People who are not recycling do not know the hazards they are causing everywhere.
Due to the fact that there is a huge problem with garbage disposal, government representatives must contribute to resolving this issue. Efficient waste management approaches help with reducing and avoiding unpleasant impacts on the environment and human health, while allowing for financial development and progress in the quality of people’s lives. People do not even imagine the size and capacity of their activities and the impact they produce on the environment. Garbage is an important ecological problem. It seems amazing that approximately all of the citizens of the world identify rubbish as a major environmental problem and yet these people still litter.