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In India the region that is dominated by denuded rocks is
  • a)
    himalayan region.
  • b)
    peninsular region.
  • c)
    valleys.
  • d)
    plateaus.
Correct answer is option 'B'. Can you explain this answer?
Most Upvoted Answer
In India the region that is dominated by denuded rocks isa)himalayan r...
Peninsular region of India dominated by denuded rocks

The peninsular region of India is dominated by denuded rocks. Let's understand this in detail.

What is the peninsular region of India?

The peninsular region of India comprises the Deccan Plateau and the adjoining mountain ranges. The Deccan Plateau is a large plateau that occupies most of the southern part of India. It is bounded by the Eastern Ghats in the east, the Western Ghats in the west, and the Satpura Range in the north.

What are denuded rocks?

Denuded rocks are rocks that have been exposed to weathering, erosion, and other natural processes that have caused them to lose their original surface features. These rocks are often characterized by a smooth, rounded surface that is the result of the action of wind, water, and other natural forces.

Why is the peninsular region of India dominated by denuded rocks?

The peninsular region of India has a long geological history that has resulted in the formation of a variety of rock types. Over time, these rocks have been exposed to weathering and erosion, which has caused them to lose their original surface features and become denuded. The region is also characterized by a relatively dry climate, which has further contributed to the denudation of the rocks.

Conclusion

In conclusion, the peninsular region of India is dominated by denuded rocks due to its long geological history, exposure to weathering and erosion, and relatively dry climate.
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In India the region that is dominated by denuded rocks isa)himalayan r...
This is the oldest part of India and therefore rocks found here are highly denuded.
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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.

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. What is the general elevation of the Peninsular Plateau in India?

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. ____ is one of the oldest and the most stable landmass of India.

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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In India the region that is dominated by denuded rocks isa)himalayan region.b)peninsular region.c)valleys.d)plateaus.Correct answer is option 'B'. Can you explain this answer?
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