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Ravines are widespread in the
  • a)
    Kashmir valley.
  • b)
    Chambal basin.
  • c)
    Gangetic plains.
  • d)
    Western ghats.
Correct answer is option 'B'. Can you explain this answer?
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Ravines are widespread in thea)Kashmir valley.b)Chambal basin.c)Ganget...
A region with a large number of deep gullies or ravines is called a badland topography. Ravines are widespread in the Chambal basin. Besides this, they are also found in Tamil Nadu and West Bengal. The country is losing about 8,000 hectares of land to ravines every year.
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Ravines are widespread in thea)Kashmir valley.b)Chambal basin.c)Ganget...
A region with a large number of deep gullies called as Ravines . These are widespread in the Chambal basin.
so the correct answer is B.
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Ravines are widespread in thea)Kashmir valley.b)Chambal basin.c)Ganget...
Ravines are widespread in the Chambal basin.

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Explanation:
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Ravines, also known as gullies or badlands, are deep and narrow erosional features formed by the continuous action of running water on soft sedimentary rocks. They are characterized by steep slopes and sharp, irregular sides. Ravines are commonly found in areas with low rainfall, sparse vegetation, and easily erodible soil.

The Chambal basin is a region located in northern India, primarily in the states of Madhya Pradesh and Rajasthan. It stretches along the Chambal River, which is a tributary of the Yamuna River. The Chambal basin is known for its rugged topography, with ravines being a prominent feature of the landscape.

Here are some reasons why ravines are widespread in the Chambal basin:

1. Geological Composition: The Chambal basin is primarily made up of soft sedimentary rocks, such as sandstone and shale. These rocks are easily eroded by the force of water, leading to the formation of ravines.

2. Lack of Vegetation: The Chambal basin has a semi-arid climate, with low rainfall and limited vegetation cover. The absence of dense vegetation results in less protection against erosion, allowing ravines to form more easily.

3. Erosion by the Chambal River: The Chambal River, with its strong current and high sediment load, plays a significant role in the formation of ravines. As the river cuts through the landscape, it erodes the soft rocks and creates deep channels or gullies.

4. Human Activities: Human activities, such as deforestation, overgrazing, and improper agricultural practices, can accelerate erosion in the Chambal basin. These activities remove the natural vegetation cover and disturb the soil, making it more susceptible to erosion and the formation of ravines.

Overall, the Chambal basin's geological composition, lack of vegetation, erosion by the Chambal River, and human activities contribute to the widespread presence of ravines in the region. These ravines not only shape the landscape but also have ecological and socio-economic implications for the local communities.
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Direction: Read the case study given below and answer any three of the questions that follow.Rising from the height of 150 m above the river plains up to an elevation of 600-900 m is the irregular triangle known as the Peninsular Plateau. Delhi ridge in the northwest, (extension of Aravalis), the Rajmahal hills in the east, Gir range in the west and the Cardamom hills in the south constitute the outer extent of the Peninsular plateau. However, an extension of this is also seen in the northeast, in the form of Shillong and Karbi-Anglong plateau. The Peninsular India is made up of a series of patland plateaus such as the Hazaribagh plateau, the Palamu plateau, the Ranchi plateau, the Malwa plateau, the Coimbatore plateau and the Karnataka plateau, etc. This is one of the oldest and the most stable landmass of India. The general elevation of the plateau is from the west to the east, which is also proved by the pattern of the flow of rivers. Some of the important physiographic features of this region are tors, block mountains, rift valleys, spurs, bare rocky structures, series of hummocky hills and wall-like quartzite dykes offering natural sites for water storage. The western and north western part of the plateau has an emphatic presence of black soil. This Peninsular plateau has under gone recurrent phases of upliftment and submergence accompanied by crustal faulting and fractures. (The Bhima fault needs special mention, because of its recurrent seismic activities). These spatial variations have brought in elements of diversity in the relief of the Peninsular plateau. The north western part of the plateau has a complex relief of ravines and gorges. The ravines of Chambal, Bhind and Morena are some of the well-known examples.Q. The western and north western part of the plateau has an emphatic presence of ______ soil.

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Direction: Read the case study given below and answer any three of the questions that follow.Rising from the height of 150 m above the river plains up to an elevation of 600-900 m is the irregular triangle known as the Peninsular Plateau. Delhi ridge in the northwest, (extension of Aravalis), the Rajmahal hills in the east, Gir range in the west and the Cardamom hills in the south constitute the outer extent of the Peninsular plateau. However, an extension of this is also seen in the northeast, in the form of Shillong and Karbi-Anglong plateau. The Peninsular India is made up of a series of patland plateaus such as the Hazaribagh plateau, the Palamu plateau, the Ranchi plateau, the Malwa plateau, the Coimbatore plateau and the Karnataka plateau, etc. This is one of the oldest and the most stable landmass of India. The general elevation of the plateau is from the west to the east, which is also proved by the pattern of the flow of rivers. Some of the important physiographic features of this region are tors, block mountains, rift valleys, spurs, bare rocky structures, series of hummocky hills and wall-like quartzite dykes offering natural sites for water storage. The western and north western part of the plateau has an emphatic presence of black soil. This Peninsular plateau has under gone recurrent phases of upliftment and submergence accompanied by crustal faulting and fractures. (The Bhima fault needs special mention, because of its recurrent seismic activities). These spatial variations have brought in elements of diversity in the relief of the Peninsular plateau. The north western part of the plateau has a complex relief of ravines and gorges. The ravines of Chambal, Bhind and Morena are some of the well-known examples.Q. The __________India is made up of a series of patland plateaus such as the Hazaribagh plateau, the Palamu plateau.

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Direction: Read the case study given below and answer any three of the questions that follow.The destruction of the soil cover is described as soil erosion. The soil forming processes and the erosional processes of running water and wind go on simultaneously. But generally, there is a balance between these two processes. The rate of removal of fine particles from the surface is the same as the rate of addition of particles to the soil layer. Sometimes, such a balance is disturbed by natural or human factors, leading to a greater rate of removal of soil. Human activities too are responsible for soil erosion to a great extent. As the human population increases, the demand on the land also increases. Forest and other natural vegetation are removed for human settlement, for cultivation, for grazing animals and for various other needs. Wind and water are powerful agents of soil erosion because of their ability to remove soil and transport it. Wind erosion is significant in arid and semi-arid regions. In regions with heavy rainfall and steep slopes, erosion by running water is more significant. Water erosion which is more serious and occurs extensively in different parts of India, takes place mainly in the form of sheet and gully erosion. Sheet erosion takes place on level lands after a heavy shower and the soil removal is not easily noticeable. But it is harmful since it removes the finer and more fertile top soil. Gully erosion is common on steep slopes. Gullies deepen with rainfall, cut the agricultural lands into small fragments and make them unfit for cultivation. A region with a large number of deep gullies or ravines is called a bad land topography. Ravines are widespread, in the Chambal basin. Besides this, they are also found in Tamil Nadu and West Bengal. The country is losing about 8,000 hectares of land to ravines every year.Q. Ravines are widespread in the ________ basin.

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Ravines are widespread in thea)Kashmir valley.b)Chambal basin.c)Gangetic plains.d)Western ghats.Correct answer is option 'B'. Can you explain this answer?
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