5 example of relief features
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The structures like plateau, plains, mountains, volcanoes, Hills, valleys, cliffs etc are called as the relief features of the Earth surfaces.
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Mountains:
These are natural terrain elevations that are characterized by their altitude and slope. This type of relief occupies almost a quarter of the surface of the planet.
Most of the mountains that exist have been formed as a result of the arching and folding of the earth's crust. This process is commonly known as deformation.
The mountains are formed by several parts. One of them is the foot, which is the lowest part. The top is the highest part and the slope or skirt is the sloping part of the mountain, which is located between the foot and the top. There are also the valleys, which are the part of land between two mountains. The mountains are grouped in different ways:
Mountain range : This is a succession of large mountains that are linked together. The mountain chains have arisen after the folding of some areas in which has accumulated great amount of sediments. Once these are compressed, the ridges are folded and created
Mountain range : The mountains appear in the same way as the mountain ranges. However, in this case it is a succession of smaller mountains
System : Is known like mountainous system to a set of mountain ranges and mountain ranges
2- Hills or hills
The 21 Types of Relief and its Features (with Images) 1
The hills or hills are also natural terrain elevations. This type of geological formation has particular characteristics in terms of form, height, etc., which allow to differentiate it from others.
Unlike the mountains, the hills usually do not exceed 100 meters in height. They are also characterized by having an extensive base, but a little steep and rounded summit.
Many specialists in the area have called the hills as ancient mountains deeply worn, either by erosion of water or wind.
3- Plains
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This type of relief is the one that is at low altitude with respect to the level of the sea. The plains can rise to 200 meters and even a little more than 300 meters.
These are extensions of flat earth or with slight undulations, which at some point are brought into contact with mountainous areas.
A plain is a field that has neither highs nor lows, which means that it is an equal surface in all its extension.
Within the plains are those created by Diastrophism , Among which are the coastal plains and the interior plains. There are also those of geomorphological origin, which are the sedimentary plains and the plains on metamorphic rocks. Then there are the so-called extensive plains.
4- Plateaus
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Plateaus, also called high plateaus, are large, slightly undulating flat terrain. They are higher than the plains and are usually between 200 and 5000 meters above sea level.
In addition to the height, the plateaus differ from the plains because the former are higher than the rest of the territory around them. This type of relief is born as a result of the erosion of old mountain systems or by the action of tectonic forces.
Depending on their location, plateaus can be classified in three ways. The first is the intramontane, which is formed together with mountains and is surrounded by them, either totally or partially.
The second is Piedmont, comprising those between the mountains and the ocean. Finally, there are the continental plateaus, which are the plateaus that rise abruptly, either from the coastal plains or from the sea.
5- Valleys
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The valleys are those areas between mountainous alignments that usually runs a river in the lower part. In fact, it is precisely because of the erosive action of this fluvial course that the valleys are formed.
They can also be formed by tectonic movements or the melting of a glacier. This type of relief is basically a terrain that is sunk in the surrounding terrain, which can be occupied by mountains or mountain ranges. There are at least eight types of valleys. Hope you like it mark it as brainliest