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Subjects

Geography

Role of Rivers

In Class 9 Geography, this topic from the chapter “Drainage” explains how rivers shape the land through erosion, transportation and deposition. Students learn how river systems and drainage patterns influence plains, valleys, agriculture, settlements, transport and the availability of water. The topic also highlights the importance of rivers in human life, along with challenges such as pollution, floods and the need for careful conservation and management of river resources.

Expert · Level 3 · 25 questions

TOPIC PRACTICE

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  1. Steep gradient and high velocity
  2. Flat plain and slow current
  3. Low water and high deposition
  4. Calm mouth and tidal influence
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  1. Because the river only cuts downward
  2. Because lateral erosion and deposition occur together
  3. Because river water always freezes
  4. Because sea waves push the river backward
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  1. Steep gradient and deep erosion
  2. Low silt and strong waves
  3. High sediment and calm sea water
  4. Dry climate and glaciers
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  1. They always make soil saline
  2. They destroy all crops
  3. They increase mountain height
  4. They increase fertility by adding new alluvial layers
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  1. Water, fertile soil and movement facility
  2. Permanently icy land
  3. Spread of dense deserts
  4. Abundance of volcanic ash
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  1. Because the river always dries up
  2. Because the raised river bed can reduce water holding capacity
  3. Because the sea instantly freezes
  4. Because mountains stop the river
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  1. Very steep slope and waterfalls
  2. Seasonal water and shallow bed
  3. Deep, wide and steady flow
  4. Dry channel and rocky bed
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  1. Because it only builds one dam
  2. Because it only increases tourism
  3. Because it is only for fishing
  4. Because it helps in irrigation, power, flood control and water supply
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  1. Water pollution and impact on aquatic life
  2. River rising into the sky
  3. Delta becoming a mountain
  4. Disappearance of all silt
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  1. They always stop the main river
  2. They add water and sediment to the main river
  3. They dry the sea
  4. They end rainfall
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  1. Direct vertical erosion
  2. Glacial deposition
  3. Lava flow
  4. Cutting off of a meander
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  1. Because it blocks the river’s spread zone during floods
  2. Because river water always decreases
  3. Because snow increases on mountains
  4. Because the sea retreats
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  1. Fertile silt deposition in floodplains may increase
  2. Deposition in floodplains and deltas may decrease
  3. The delta may expand more rapidly
  4. Rainfall may stop in the downstream region
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  1. River water staying permanently in the sky
  2. All water instantly becoming saline in the sea
  3. Water seeping through the river bed and banks
  4. River turning into stone
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  1. Permanent freezing of water into ice
  2. Ending of sea tides
  3. River flowing uphill
  4. Soil erosion, increased silt and flood risk
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  1. Due to height difference and fast flow
  2. Due to excessive sand deposition
  3. Due to sea tides
  4. Due to drying of the river
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  1. Sea becoming a mountain
  2. Waterlogging and salinity
  3. All rivers becoming sweet
  4. Permanent stoppage of rainfall
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  1. Increasing bank erosion
  2. Damaging settlements by flood
  3. Forming alluvial plains and deltas
  4. Spreading polluted water
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  1. Depositing fertile alluvium
  2. Providing fish resources
  3. Providing irrigation water
  4. Causing damage through floods and bank erosion
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  1. Because water, land and human use are connected in one system
  2. Because a river basin has no population
  3. Because it depends only on marine fish
  4. Because it only tells mountain height
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  1. Erosion of rocks by glaciers
  2. Deposition of relatively heavier sediments near river banks during floods
  3. Erosion of coastal rocks by sea waves
  4. Deposition of sand dunes by wind
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  1. Because sand blocks the sun
  2. Because sand makes the sea fresh
  3. Because sand produces rainfall
  4. Because the structure of the river bed and banks weakens
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  1. Need for treatment increases
  2. Water always becomes safer
  3. River immediately dries up
  4. Silt completely disappears
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  1. When silt is very high and sea is calm
  2. When tides and waves remove deposits
  3. When the river has no mouth
  4. When the river ends only in a lake
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  1. The river loses most of its water downstream
  2. The sea pushes particles towards the upper course of the river
  3. Larger, heavier particles are deposited earlier, while finer particles are carried farther
  4. The Sun's heat burns all large particles into smaller ones

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