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Subjects

Geography

The Himalayan Rivers

In Class 9 Geography, this topic from the chapter “Drainage” introduces the Himalayan river systems, especially the Indus, Ganga and Brahmaputra. Students learn how these rivers are fed by glaciers, snow and rainfall, making them largely perennial, and trace their courses, major tributaries and drainage patterns. The topic also explains how Himalayan rivers shape deep gorges, valleys, meanders, floodplains and deltas, while supporting farming, settlements and ecosystems. It highlights their economic importance as well as the challenges of floods, erosion and changing water conditions.

Hard · Level 4 · 25 questions

TOPIC PRACTICE

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  1. Steep slope and fast water flow
  2. Very low velocity and flat bed
  3. River ending in desert
  4. Entry of sea waves
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  1. Deltas form by erosion and gorges by deposition
  2. Deltas form by deposition and gorges by vertical erosion
  3. Both form only by wind action
  4. Both form by marine corals
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  1. Their source region and flow direction
  2. Their colour and taste
  3. Guessing length without map
  4. Only hearing their names
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  1. Fine alluvial sediment is deposited and soil becomes fertile
  2. All soil permanently turns into stone
  3. Soil completely disappears
  4. Only marine sand is deposited
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  1. Influence of river deposition and tidal coastal conditions
  2. Complete dominance of desert aridity
  3. Permanent spread of glacial ice
  4. Only plateau lava region
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  1. Jamuna is the Brahmaputra's name in Bangladesh and Yamuna is a tributary of Ganga
  2. Both are branches of the Indus
  3. Both are only ocean currents
  4. Yamuna is the Tibetan name of Brahmaputra
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  1. It forms a delta in the Bay of Bengal
  2. It drains on India's eastern coast
  3. It carries water through the north-west toward the Arabian Sea
  4. It completely joins the Ganga
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  1. They collect water from large areas and support irrigation and settlement
  2. They stop all water from reaching the sea
  3. They only create deserts
  4. They make rivers seasonal
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  1. In the lower delta region
  2. In the upper mountainous course
  3. On the marine continental shelf
  4. Among stagnant lakes
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  1. Low slope, high sediment and floods
  2. High sea waves and corals
  3. Permanent ice and no water
  4. Volcanic eruption and lava
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  1. Nepal and Himalayan region
  2. Coastal Kerala
  3. Thar Desert
  4. Western Malwa plateau
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  1. Expansion of a main river by tributaries
  2. Birth of a river in the sea
  3. Formation of a river by wind
  4. River being an artificial canal
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  1. Peninsular rivers are mostly rain-fed and flow in relatively older valleys
  2. Peninsular rivers always originate from glaciers
  3. Himalayan rivers never flow in plains
  4. There is no geographical difference between them
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  1. Low slope, high silt and slow flow
  2. Steep mountain slope and hard glaciers
  3. High plateau far from the sea
  4. Complete absence of water
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  1. They attract settlement through irrigation, fertile soil and water availability
  2. They permanently stop all settlement
  3. They only create seaports
  4. They make plains waterless
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  1. Because they also provide fertile sediment, irrigation and water resources
  2. Because they never flood
  3. Because they contain only sea water
  4. Because they do not flow in India
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  1. Indus river system
  2. Brahmaputra river system
  3. Kaveri river system
  4. Luni river system
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  1. The Ganga system connects rivers from diverse geographical regions
  2. The Ganga system has no tributaries
  3. The Ganga flows only in Tibet
  4. The Ganga's mouth is in the Arabian Sea
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  1. Deposition of sediment in the channel and division of streams
  2. River originating in the sea
  3. Glacier remaining always fixed
  4. Blowing of desert sand
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  1. Because direction, tributaries, landforms and uses change along the course
  2. Because only the river name is enough
  3. Because the mouth comes before the source
  4. Because all rivers have equal length
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  1. Changes in glacier melt rate and seasonal balance of river flow
  2. Rivers immediately becoming marine corals
  3. All rivers shifting to the Western Ghats
  4. Gravity ending in rivers
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  1. New deposited landforms and distributaries may form
  2. The coastline always becomes mountains
  3. The sea completely dries up
  4. River water flows upward
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  1. Main channel splitting into branches due to sediment deposition
  2. Increase in vertical erosion
  3. River flowing back toward mountains
  4. Glacier turning into desert
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  1. Reduced slope and velocity lower the river's carrying capacity
  2. Sea tide pushes the river upward
  3. Water fully turns into ice
  4. The source changes into a desert
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  1. They are short and isolated drains
  2. They form extensive river systems affecting large plains
  3. They are only coastal lagoons
  4. They are rivers without sources

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