Landforms

ICSE Class 6 Geography · Solutions for Goyal Brothers Prakashan Geography by Veena Bhargava Class 6 ICSE · 31 solved questions

Exercise
1Tick the right option

One of the following is an old fold mountain

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Aravallis

2Tick the right option

Tibetan plateau is a

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Intermontane plateau

3Tick the right option

Block mountains are formed due to

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faulting

4Tick the right option

Gangetic plains are formed by

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deposition

5Tick the right option

These are surrounded by mountain ranges on one side and plain or ocean on the opposite side

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border plateau

6Tick the right option

Compressional forces may lead to the formation of

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fold mountains

7Tick the right option

Anticline is the upraised part of a ............... .

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fold

8Tick the right option

Fold mountains are mostly constituted of ............... rocks.

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sedimentary

9Tick the right option

Horst is the result of

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faulting

10Tick the right option

It releases gas, ash, solid rocks and lava

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volcano

11Tick the right option

Volcanic eruption and earthquakes are part of which force

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endogenic forces

12Tick the right option

Which is not a volcanic mountain?

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Mt. Everest

13Tick the right option

Plains formed as a result of emergence of sea bottom are

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structural plains

14Tick the right option

Which is not an example of old fold mountain?

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Himalayas

1Fill in the blanks

Young fold mountains have ............... peaks.

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Young fold mountains have pointed peaks.

2Fill in the blanks

Most of the plateaus are storehouse of ............... .

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Most of the plateaus are storehouse of minerals.

3Fill in the blanks

Rift valley is located between two ............... .

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Rift valley is located between two parallel faults.

4Fill in the blanks

Appalachians are example of ............... fold mountains.

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Appalachians are example of old fold mountains.

1Differentiate between

Old fold and young fold mountains

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Sl.
No.
Old fold mountainsYoung fold mountains
1.They are lower in height.They are very high mountains.
2.They have rounded peaks and gentle slopes.They have pointed peaks and steep slopes.
3.Examples: The Appalachians in North America, the Urals in EuropeExamples: The Himalayas in India, the Rockies in North America.
2Differentiate between

Rift Valley and block mountains

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Sl.
No.
Rift ValleyBlock Mountains
1.Rift Valley is a lowland region that forms where earth's tectonic plates move apart or rift.Block Mountains are formed as a result of faulting.
2.Rift Valley is bordered by faults zones and separated by land masses.Block Mountains have steep sides, flat top and are enclosed by faults.
3.Examples: Vosges in France, Vindhyas in IndiaExamples: Rhine Valley of River Rhine, Rift Valley of river Narmada.
3Differentiate between

Erosional plains and depositional plains

Sl.
No.
Erosional PlainsDepositional Plains
1.Erosional Plains are formed as a result of erosion by running water, wind and rivers.Depositional Plains are formed as a result of deposition of sediments brought by rivers.
2.Example: Plains around Aravalli regionExample: Indo-Gangetic plains in India.

Solution not available in the source paper.

4Differentiate between

Intermontane and piedmont plateaus

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Sl.
No.
Intermontane PlateausPiedmont Plateaus
1.Intermontane Plateau is situated between two or more mountain ranges.Piedmont Plateau is surrounded by mountain ranges on one side and bounded by a plain or an ocean on the opposite side.
2.Example: Tibetan PlateauExample: Patagonian Plateau
1Answer in brief

How are fold mountains formed? Give two examples of fold mountains?

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The fold mountains are formed when earth's movement throws massive folds or ridges which form the mountains. These movements of earth are primarily horizontal movement and cause 'wrinkles' or 'folds'. The upraised parts of the folds are called anticlines and downward folds are called synclines. Two example of fold mountains are:

  1. The Himalayas in India
  2. Rockies in North America
2Answer in brief

State two characteristics of block mountains.

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Two characteristics of block mountains are:

  1. Block mountains are steep sided and flat topped.
  2. Block mountains are characterised by massiveness, steep slopes and comparatively smooth topography.
3Answer in brief

How are rift valleys formed? Give one example of rift valley.

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A Rift Valley is formed when earth's tectonic plates move apart or rift. It is a linear depression or trough created by the sinking of the intermediate crustal rocks between two or more parallel faults. Rhine Valley is one of the examples of Rift Valley.

4Answer in brief

Compare life in the mountains and in the plains.

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Sl.
No.
Life in the mountainsLife in the plains
1.People face the problem of conveyance as these regions are not well connected by roadways, railways and airways.Conveyance is easy for people as levelled land makes it easy to construct roads and railway lines.
2.People have to face environmental and economical difficulties. There is sparse populationThe fertile land promotes agriculture and irrigation is also cheap. It supports dense population.
3.They are centres of mining as they are rich in deposits of minerals.Agriculture is the most important occupation.
5Answer in brief

What type of mountain is Mt. Kilimanjaro?

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Mt. Kilimanjaro is a Volcanic mountain.

6Answer in brief

Define structural plains.

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The plains that are formed as a result of emergence of sea bottom near coast are known as structural plains.

1Give reasons

Young fold mountains have high peaks

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Young fold mountains have high and pointed peaks because they are younger and have not been much eroded by wind or water. On the contrary, old fold mountains have been subjected to the forces of denudation (such as weather, rivers, glaciers) for a longer geological period. Due to this prolonged erosion, they are lower in height and have round peaks.

2Give reasons

Tibetan plateau is surrounded by mountains.

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Tibetan plateau is an example of Intermontane plateau as it is surrounded by the Himalayas and the Kunlun mountains.

3Give reasons

Rift valley have steep sides

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Rift valley have steep sides because they are formed as a linear depression or trough by the sinking of the intermediate crustal rocks between two or more parallel faults. Sudden rifting of tectonic plates leads to steep sides of Rift valley.

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