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Effects of soil erosion Essay
5 disadvantages of soil erosion
5 disadvantages of soil erosion
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What is Soil Erosion?
Soil erosion is when soil moves (like a slope) to a different place. It can be a short distance or kilometers carried by rivers. Soil erosion is occurring by winds, rains, floods, glaciers, rivers, and earthquakes. Soil erosion is a natural occurring process which affects all landforms. The soil that is moved goes down the flattered land in which it may block roads and damage houses. It enters the streams and rivers in which it harms wildlife and makes water dirty and goes out to the sea. In agriculture, soil erosion is wearing away of a field's topsoil by natural physical forces of water and the wind or farming activities such as tillage. Erosion involves three distinct actions, soil detachment, movement, and deposition.
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Rill erosion is when on sloping land, the water that runs off may gather in small V-shaped rolls. Gully erosion occurs on spread subsoils. These are mostly deep and create a lot of sediment, which often feeds into rivers. Mass-movement erosions when gravity combines with heavy rain or earthquakes and the whole slopes can slump, slip or slide. Slips are one of the main forms of erosion in the North Island. They are a direct result of the change from forest to pasture. Slips occur when the soil (topsoil and subsoil) on slopes becomes saturated.Slips are common, where the underlying rock is mudstone or siltstone. In the South Island, soil slips are widespread throughout the hill country (Gisborne, Taihape, Wanganui, Taranaki and King Country), but mostly north of Christchurch. Streambank erosion is common throughout New Zealand, especially in rivers and watercourses with periodic flooding. I chose this topic because it is one of the main crisis in NZ. It will affect our future if we don’t take action now. New Zealand loses 200 - 300 million tonnes of soil every year in the ocean. The rate of of soil erosion is New Zealand is about ten times faster than the rest of the world. If we don’t start taking action, then our crops, plants and trees will start dying, New Zealand will be
Yes this feature is the result of erosion and depositional processes however, it is not associated with the current water course. This feature may be the result of a Gilbert type delta that once occupied this area. Gilbert type deltas have three main components; topsets, foresets and bottomsets. Topsets are fluvial sediments (primarily sandur deposits) that were deposited on the subaerial delta surface. Erosive events occurring on the upper forslope can result in downslope channels and chutes. These features are then eroded by either strong currents or by debris flow resulting in these channels and chutes to become filled. Foresets are a combination of sand and gravel facies. The are deposited by gravitational processes on the delta foreslope and the grains tend to become finer and more angular downslope. Bottomsets consist of fine grained silts and clay and are deposited at the foot of the delta front.
1. 225 MY : Weathering and erosion of very old folded rocks on an area
Longshore drift influences the deposition and erosion of sediments. Waves erode the coast and transport the eroded material along the coastline. Over a period of time, the material will be deposited on a beach or form a larger feature such as a spit. Groynes are structures built at equal intervals along the coastline. Their purpose is to restrict longshore drift, preventing coastal erosion.
There are three clear landslides; the southwest landslide is stream-laid sand and gravel from the quaternary that was located on a steep slope resulting in gravity pulling sediments down the steep slope. The northeast landslide appears to be tuff sediments that have fallen upon biotite-quartz diorite rocks. The northwestern landslide is the largest of the landslides. The landslide occurred just south of the creek; erosion must have lowered the creeks elevation creating a steep decline resulting in Bena gravel to fall.
Removing vegetation removes the root systems, which help hold soil in place. Running water can now more easily wash soil and rock away, increasing erosion.
Erosion is when the elements such as wind, water, and ice remove pieces of land. (“What is Coastal Erosion?”) Coastal Erosion takes place when destructive waves wear parts of the coast away. Four ways in which this takes place are corrasion/abrasion, hydraulic action, attrition, and corrosion/solution. (“Internet Geography”) Corrasion/abrasion is when materials are hurled at the base of cliffs through waves. Hydraulic action is when waves hit the base of a cliff and air is compacted, when the wave leaves air is rushed out and often this causes the material to break. Attrition is when the waves cause rocks and pebbles to smash into each other and eventually break into pieces. Finally, Corrosion/solution is when certain types of cliff erode from the result of acids in the sea. (“Internet Geography”) Coastal Erosion is the natural process of taking land away permanently from one place to put it somewhere else. (“What is Coastal Erosion?”) Eroding coastlines are an abundant and important topic because it can change people’s surroundings in a negative way. I would like to address the questions surrounding Coastal Erosion.
Soil liquefaction describes a phenomenon whereby a saturated or partially saturated soil substantially loses strength and stiffness in response to an applied stress, usually earthquake shaking or other sudden change in stress condition, causing it to behave like a liquid. The phenomenon is most often observed in saturated, loose (low density), sandy soils. This is because the loose sand has a tendency to compress when a load is applied; dense sands by contrast tend to expand in volume. If the soil is saturated by water, then water fills the gaps between soil grains. In response to the soil compressing, this water increases in pressure and attempts to flow out from the soil to zones of low pressure (usually upward towards the ground surface). However, if the loading is rapidly applied and large enough, or is repeated many times (e.g. earthquake shaking, storm wave loading) such that it does not flow out in time before the next cycle of load is applied, the water pressures may build to an extent where they exceed the contact stresses between the grains of soil that keep them in contact with each other. These contacts between grains are the means by which the weight from buildings and overlying soil layers are transferred from the ground surface to layers of soil or rock at greater depths. This loss of soil structure causes it to lose all of its strength. According to the
The rivers and creeks along the wet tropics in far North Queensland are followed by massive amounts of banana farms. These farms run across 1500 kilometres of the Queensland coastline. During heavy rainfall, which is plentiful in the area, sediment and nutrients run off into the rivers and eventually end up in the Great Barrier Reef. One of the biggest threats to the Reef is Johnstone River, as it is one of the closest rivers to the Reef, and the farms along its coast are producing the highest yields. Banana farms are used very intensely and combined with the plentiful floods in the area, sediment runoff from the farms is at an all-time
is being eroded by the sea so that cliffs, up to 20 metres high rise
eroded as fast as 6 metres per year, but the average is 1.8 metres per
Mudslides usually occur in hilly areas, for an example, when there was a mudslide in Bangladesh few months back, it occurred at Chittagong. Mudslides occur when a portion of a hill side becomes too weak to hold up its own weight. This is generally caused by an intense amount of rain fall. With all of the new water introduced into the slope the content of liquid makes it so heavy that gravity pulls it downward. Although water plays a major factor in creating the mud that flows in a mudslide the real reason that the land begins to slide is gravity. What happens is mudslides redistribute soil and sediments in a process that can be in abrupt collapses or in slow gradual slides.
Coastal Erosion is a process at Muriwai that gradually wears away the rock particles of the earth's surface, transporting them to another location. There are many types of processes that cause erosion at Muriwai such as wave erosion, wind erosion and wave refraction.
Slope stability is the potential of soil covered slopes to withstand and undergo movement. Stability is determined by the balance of shear stress and shear strength. A previously stable slope may be initially affected by preparatory factors, making the slope conditionally unstable. Triggering factors of a slope failure can be climatic events can then make a slope actively unstable, leading to mass movements. Mass movements can be caused by increase in shear stress, such as loading, lateral pressure, and transient forces. Alternatively, shear strength may be decreased by weathering, changes in pore water pressure, and organic material.
Agriculture also leads to soil erosion, both through rainfall and wind. This soil can damage the aquatic ecosystems it ends up in, an...
There are many different glacial landforms created by glacial erosion, one of these landforms is U-shaped valleys or glacial troughs. This glacial landform has many distinct characteristics. One of these characteristics is that it has very steep valley sides caused by the glacier as it moves down the valley eroding the sides of the valley by the processes of abrasion and plucking. Abrasion is when the boulders and moraine carried by the glacier rubs and erodes the valley side as it physically moves down the valley. Plucking happens when the water in the glacier freezes inside of the cracks in the individual rocks on the valley side then the water freezes and as the glacier moves the rock is plucked or torn from the valley side producing the steep side to the valley.