Consider the following pairs related to geomorphic features formed by running water:1. Peneplain : A nearly level plain formed by wind erosion.2. Gorge : A deep valley with steep sides, often formed by a river.3. Plunge Pool : A deep hole at the base of a waterfall formed by the impact of water.4. Canyon : A narrow valley with steep, step-like sides, wider at the top than at the bottom.How many pairs given above are correctly matched?a)Only one pairb)Only two pairsc)Only three pairsd)All four pairsCorrect answer is option 'C'. Can you explain this answer?

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Consider the following pairs related to geomorphic features formed by running water:

1. Peneplain : A nearly level plain formed by wind erosion.

2. Gorge : A deep valley with steep sides, often formed by a river.

3. Plunge Pool : A deep hole at the base of a waterfall formed by the impact of water.

4. Canyon : A narrow valley with steep, step-like sides, wider at the top than at the bottom.

How many pairs given above are correctly matched?

a)
Only one pair
b)
Only two pairs
c)
Only three pairs
d)
All four pairs

Correct answer is option 'C'. Can you explain this answer?

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Verified Answer

Consider the following pairs related to geomorphic features formed by...

1. Peneplain : Incorrect. A peneplain is a nearly level plain formed by extensive stream erosion, not wind erosion.

2. Gorge : Correct. A gorge is a deep valley with very steep to straight sides, often formed by a river.

3. Plunge Pool : Correct. A plunge pool is a deep hole at the base of a waterfall, formed by the impact of water and the rotation of boulders.

4. Canyon : Correct. A canyon is a narrow valley with steep, step-like sides, which is wider at the top than at the bottom, typically formed by a river cutting through horizontal bedded sedimentary rocks.

Thus, three pairs are correctly matched, making Option C the correct answer.

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Consider the following pairs related to geomorphic features formed by...

Explanation:

1. Peneplain
A peneplain is a nearly level plain that has been worn down by erosion. However, it is not formed by wind erosion but rather by the action of running water over a long period of time.

2. Gorge
A gorge is indeed a deep valley with steep sides, often formed by a river. The flowing water erodes the land, creating a narrow and deep valley over time.

3. Plunge Pool
A plunge pool is a deep hole at the base of a waterfall formed by the impact of water. As the water falls from a height, it erodes the rock below, creating a deep pool at the base of the waterfall.

4. Canyon
A canyon is a narrow valley with steep, step-like sides, wider at the top than at the bottom. Canyons are typically formed by the erosion of rivers cutting through rock over millions of years.
Therefore, out of the given pairs, three of them are correctly matched: Gorge, Plunge Pool, and Canyon. The only incorrect pair is Peneplain, as it is not formed by wind erosion but by the action of running water.

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Consider the following statements:1. Landforms undergo three stages called youth, mature, and old stages.2. Running water is the primary geomorphic agent in regions with high humidity and heavy rainfall.3. Erosional landforms created by running water are predominantly associated with mature rivers flowing over gentle gradients.Which of the statements given above is/are correct?

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Direction: Read the case study given below and answer any three of the questions that follow.In humid regions, which receive heavy rainfall, running water is considered the most important of the geomorphic agents in bringing about the degradation of the land surface. There are two components of running water. One is overland flow on the general land surface as a sheet. Another is linear flow as streams and rivers in valleys. Most of the erosional landforms made by running water are associated with vigorous and youthful rivers flowing over steep gradients. With time, stream channels over steep gradients turn gentler due to continued erosion, and as a consequence, lose their velocity, facilitating active deposition. There may be depositional forms associated with streams flowing over steep slopes. But these phenomena will be on a small scale compared to those associated with rivers flowing over medium to gentle slopes. The gentler the river channels in gradient or slope, the greater is the deposition. When the stream beds turn gentler due to continued erosion, downward cutting becomes less dominant and lateral erosion of banks increases and as a consequence the hills and valleys are reduced to plains.Q. What happens when the stream beds turn gentler due to continued erosion?

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Direction: Read the case study given below and answer any three of the questions that follow.In humid regions, which receive heavy rainfall running water is considered the most important of the geomorphic agents in bringing about the degradation of the land surface. There are two components of running water. One is overland flow on general land surface as a sheet. Another is linear flow as streams and rivers in valleys. Most of the erosional landforms made by running water are associated with vigorous and youthful rivers flowing over steep gradients. With time, stream channels over steep gradients turn gentler due to continued erosion, and as a consequence, lose their velocity, facilitating active deposition. There may be depositional forms associated with streams flowing over steep slopes. But these phenomena will be on a small scale compared to those associated with rivers flowing over medium to gentle slopes. The gentler the river channels in gradient or slope, the greater is the deposition. When the stream beds turn gentler due to continued erosion, downward cutting becomes less dominant and lateral erosion of banks increases and as a consequence the hills and valleys are reduced to plains.Q. The gentler the river channels in gradient or slope, the greater is the ___________.

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Direction: Read the case study given below and answer any three of the questions that follow.In humid regions, which receive heavy rainfall running water is considered the most important of the geomorphic agents in bringing about the degradation of the land surface. There are two components of running water. One is overland flow on general land surface as a sheet. Another is linear flow as streams and rivers in valleys. Most of the erosional landforms made by running water are associated with vigorous and youthful rivers flowing over steep gradients. With time, stream channels over steep gradients turn gentler due to continued erosion, and as a consequence, lose their velocity, facilitating active deposition. There may be depositional forms associated with streams flowing over steep slopes. But these phenomena will be on a small scale compared to those associated with rivers flowing over medium to gentle slopes. The gentler the river channels in gradient or slope, the greater is the deposition. When the stream beds turn gentler due to continued erosion, downward cutting becomes less dominant and lateral erosion of banks increases and as a consequence the hills and valleys are reduced to plains.Q. Why do stream channels over steep gradients turn gentler with time?

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Direction: Read the case study given below and answer any three of the questions that follow.In humid regions, which receive heavy rainfall running water is considered the most important of the geomorphic agents in bringing about the degradation of the land surface. There are two components of running water. One is overland flow on general land surface as a sheet. Another is linear flow as streams and rivers in valleys. Most of the erosional landforms made by running water are associated with vigorous and youthful rivers flowing over steep gradients. With time, stream channels over steep gradients turn gentler due to continued erosion, and as a consequence, lose their velocity, facilitating active deposition. There may be depositional forms associated with streams flowing over steep slopes. But these phenomena will be on a small scale compared to those associated with rivers flowing over medium to gentle slopes. The gentler the river channels in gradient or slope, the greater is the deposition. When the stream beds turn gentler due to continued erosion, downward cutting becomes less dominant and lateral erosion of banks increases and as a consequence the hills and valleys are reduced to plains.Q. Why do stream channels over steep gradients turn gentler with time?

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Consider the following pairs related to geomorphic features formed by running water:1. Peneplain : A nearly level plain formed by wind erosion.2. Gorge : A deep valley with steep sides, often formed by a river.3. Plunge Pool : A deep hole at the base of a waterfall formed by the impact of water.4. Canyon : A narrow valley with steep, step-like sides, wider at the top than at the bottom.How many pairs given above are correctly matched?a)Only one pairb)Only two pairsc)Only three pairsd)All four pairsCorrect answer is option 'C'. Can you explain this answer?

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Consider the following pairs related to geomorphic features formed by running water:1. Peneplain : A nearly level plain formed by wind erosion.2. Gorge : A deep valley with steep sides, often formed by a river.3. Plunge Pool : A deep hole at the base of a waterfall formed by the impact of water.4. Canyon : A narrow valley with steep, step-like sides, wider at the top than at the bottom.How many pairs given above are correctly matched?a)Only one pairb)Only two pairsc)Only three pairsd)All four pairsCorrect answer is option 'C'. Can you explain this answer? for Humanities/Arts 2025 is part of Humanities/Arts preparation. The Question and answers have been prepared according to the Humanities/Arts exam syllabus. Information about Consider the following pairs related to geomorphic features formed by running water:1. Peneplain : A nearly level plain formed by wind erosion.2. Gorge : A deep valley with steep sides, often formed by a river.3. Plunge Pool : A deep hole at the base of a waterfall formed by the impact of water.4. Canyon : A narrow valley with steep, step-like sides, wider at the top than at the bottom.How many pairs given above are correctly matched?a)Only one pairb)Only two pairsc)Only three pairsd)All four pairsCorrect answer is option 'C'. Can you explain this answer? covers all topics & solutions for Humanities/Arts 2025 Exam. Find important definitions, questions, meanings, examples, exercises and tests below for Consider the following pairs related to geomorphic features formed by running water:1. Peneplain : A nearly level plain formed by wind erosion.2. Gorge : A deep valley with steep sides, often formed by a river.3. Plunge Pool : A deep hole at the base of a waterfall formed by the impact of water.4. Canyon : A narrow valley with steep, step-like sides, wider at the top than at the bottom.How many pairs given above are correctly matched?a)Only one pairb)Only two pairsc)Only three pairsd)All four pairsCorrect answer is option 'C'. Can you explain this answer?.

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