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In this Class 9 Geography topic from the chapter Drainage, students learn how water flows across India through river systems, drainage basins, and networks. They explore the Himalayan and Peninsular river systems, compare their origins, courses, seasonal flow, and landforms, and understand patterns such as dendritic, trellis, and radial drainage. The topic also introduces the importance of rivers and lakes, along with concerns related to floods, pollution, and water management.
TOPIC PRACTICE
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Hard · Level 29 · river system,source to mouth,study methodView options
Observing source, flow direction, tributaries and mouth
Counting only cities along the river
Observing only river colour
Observing only date of rainfall
Hard · Level 29 · ganga tributaries,yamuna,ghaghara,sonView options
Their bank positions and confluence areas should be understood separately
All three should be treated as distributaries of Indus
All three should be treated as west-flowing Peninsular rivers
All three should be called inland drainage
Hard · Level 29 · himalayan rivers,peninsular rivers,comparisonView options
Himalayan rivers are long and perennial, Peninsular rivers are mostly rainfall-based and seasonal
Both are always short and dry
Peninsular rivers get more water from glaciers
Himalayan rivers never form plains
Hard · Level 29 · trellis drainage,right angle,map clueView options
Trellis drainage
Radial drainage
Dendritic drainage
Inland drainage
Hard · Level 29 · radial drainage,plateau,central highlandView options
Radial drainage
Trellis drainage
Rectangular drainage
Delta drainage
Hard · Level 29 · alluvial soil,flood plain,delta,depositionView options
They are linked with river deposition
They form only by volcanic eruption
They form only by glaciers
They form only inside the sea
Hard · Level 29 · arabian sea,bay of bengal,external drainageView options
Because most external drainage rivers join these water bodies
Because all rivers originate from them
Because they form the Himalaya
Because they end river pollution
Hard · Level 29 · catchment area,river discharge,tributariesView options
Rainfall, snowmelt and tributaries of that area
Only colour of the sea
Only language of cities
Only mountain names
Hard · Level 29 · drainage system,basin,water divide,human impactView options
Basin, water divide, river system, flow direction and human impact
Only cities, language, food and festivals
Only mountains, minerals, industries and roads
Only sea, moon, wind and temperature
Hard · Level 29 · tributaries,river discharge,drainage basinView options
Water and sediment load in the main river may increase
The main river always dries up
The main river stops flowing towards the sea
The main river immediately becomes a glacier
Hard · Level 30 · antecedent drainage,himalayan rivers,gorgesView options
They had formed their courses before mountain uplift and kept cutting after uplift
They rise only from the sea
They are rivers of the Peninsular plateau
They do not form any valley
Hard · Level 30 · gorges,vertical erosion,himalayan drainageView options
Delta deposition
Strong vertical erosion by river
Weathering by sea waves
Desert wind deposition
Hard · Level 30 · dendritic drainage,rock resistance,slopeView options
Radial pattern
Trellis pattern
Dendritic pattern
Rectangular pattern
Hard · Level 30 · trellis drainage,structural control,tributariesView options
Because rock structure and parallel valleys control flow
Because the river freezes in the sea
Because all rivers rise from one lake
Because slope is completely absent
Hard · Level 30 · radial drainage,amarkantak,central highlandView options
Amarkantak is a low delta where all rivers meet
Amarkantak is a central highland from which rivers flow in different directions
Amarkantak is a marine estuary
Amarkantak is only a sandy inland basin
Hard · Level 30 · rectangular drainage,joints,fracturesView options
Right-angled bends and following joints
Rivers meeting only in a circular lake
River always flowing west to east
River having no tributary system
Hard · Level 30 · parallel drainage,steep slope,drainage patternView options
Closed basin with very low slope
Area with steep and almost uniform slope
Delta enclosed from all sides
Only glacial plain
Hard · Level 30 · water divide,river basin,catchmentView options
A water divide may form the basin boundary while the basin is the water collecting area
A water divide is always the river delta
A basin is found only under the sea
Both terms are synonyms of tributary
Hard · Level 30 · himalayan rivers,dynamic course,sedimentsView options
Due to young mountains higher sediments and slope changes in plains
Due to old stable plateau and low sediments
Only due to volcanic sources
Due to origin from sea water
Hard · Level 30 · peninsular rivers,stable course,old plateauView options
Old and hard nature of the Peninsular landmass
Continuous growth of Himalayan glaciers
Sea level always remaining stable
Desert sand blocking every river
Question 1HardLevel 29
What is the best way to study a river system systematically?
Correct answer: A
Studying a river system from source to mouth is the clearest method. Exam tip: study rivers systematically.
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