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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.
TOPIC PRACTICE
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Hard · Level 33 · brahmaputra,tibet,assamView options
In Tibet it receives heavy rainfall and causes floods
In Assam it dries into a small stream
Cold dry Tibet and rainy India change its water and silt load
It does not enter India
Hard · Level 33 · brahmaputra floods,assam,sedimentView options
Low rainfall and hard river bed
High rainfall, high discharge and heavy sediment
Complete drying of the river
Deposition of marine corals
Hard · Level 33 · ganga brahmaputra delta,sediment,depositionView options
Deposition of huge alluvial sediment by both rivers
Only marine volcanic activity
Erosion by desert winds
Rivers flowing without sediment
Hard · Level 33 · farakka,ganga,padma,hugliView options
It completely joins Ganga with Indus
It sends one branch as Bhagirathi-Hugli and another as Padma
It ends the Ganga in a desert
It makes the Ganga entirely underground
Hard · Level 33 · padma,jamuna,meghna,bangladeshView options
Indus route to the Arabian Sea
The combined Ganga-Brahmaputra system in Bangladesh
Yamuna route in Rajasthan
Satluj joining Kaveri
Hard · Level 33 · meanders,oxbow lake,plainsView options
Lateral erosion and deposition due to low slope in plains
Only avalanches in mountains
Reverse flow due to sea tides
River flowing without water
Hard · Level 33 · natural levees,flood deposition,river plainsView options
Repeated deposition of sediment along banks during floods
Continuous freezing of river bed
Rock cutting by sea waves
Formation of sand dunes in desert
Hard · Level 33 · kosi,course change,siltView options
Because it carries heavy silt and flows on low slope in plains
Because it flows under the sea
Because it is a waterless river
Because it is limited only to plateau
Hard · Level 33 · tributaries,drainage basin,river systemView options
The drainage basin will generally be extensive
The river system will end immediately
Water will not reach the main river
The river will always remain locked in a lake
Hard · Level 33 · river mouth,drainage direction,arabian sea,bay of bengalView options
Concept of river mouth and drainage direction
Concept of measuring mountain height
Leaf structure of forests
Soil acidity
Hard · Level 33 · alluvial plains,fertile soil,agricultureView options
Because fine alluvial soil brought by rivers is deposited there
Because only hard lava is found there
Because no river flows there
Because sea salt is always deposited
Hard · Level 33 · bhagirathi,alaknanda,ganga sourceView options
Because they are major in forming the source streams of the Ganga
Because they are western branches of the Indus
Because they are ocean currents
Because they are only desert streams
Hard · Level 33 · yamuna,yamunotri,prayagrajView options
Origin in the Himalayas and joining Ganga as a tributary
Becoming a Tibetan stream of Brahmaputra
Independently draining into the Arabian Sea
Disappearing in a desert
Hard · Level 33 · tsangpo,dihang,brahmaputraView options
A river's name and nature may change across regions
A river has no source
A river is only an artificial canal
A river does not enter the sea
Hard · Level 33 · hydropower,steep slope,himalayan riversView options
Steep slope and fast water flow
Very low velocity and flat bed
River ending in desert
Entry of sea waves
Hard · Level 33 · delta,gorge,erosion,depositionView options
Deltas form by erosion and gorges by deposition
Deltas form by deposition and gorges by vertical erosion
Both form only by wind action
Both form by marine corals
Hard · Level 33 · ganga tributaries,northern southern,source regionView options
Their source region and flow direction
Their colour and taste
Guessing length without map
Only hearing their names
Hard · Level 33 · floodplain,alluvium,fertilityView options
Fine alluvial sediment is deposited and soil becomes fertile
All soil permanently turns into stone
Soil completely disappears
Only marine sand is deposited
Hard · Level 33 · sundarban,delta,mangroveView options
Influence of river deposition and tidal coastal conditions
Complete dominance of desert aridity
Permanent spread of glacial ice
Only plateau lava region
Hard · Level 33 · jamuna,yamuna,river namesView options
Jamuna is the Brahmaputra's name in Bangladesh and Yamuna is a tributary of Ganga
Both are branches of the Indus
Both are only ocean currents
Yamuna is the Tibetan name of Brahmaputra
Question 1HardLevel 33
Which explanation correctly describes the changing nature of the Brahmaputra from Tibet to Assam?
Correct answer: C
Monsoon rainfall and tributaries in India make the Brahmaputra more water-rich. Exam tip: remember the Tibet-Assam contrast.
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