Why can the course shifting tendency of Kosi be dangerous for plains?
Course shifting can affect settlements and farms. Exam tip: connect Kosi with floods and course change.
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SubjectsGeography
हिमालयी नदियाँ
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
Up to 20 questions from this page. Select your focus, then start.
Course shifting can affect settlements and farms. Exam tip: connect Kosi with floods and course change.
View question detailsAlluvial plains provide water and fertile soil. Exam tip: connect river plains with human settlement.
View question detailsBrahmaputra changes name and character according to region. Exam tip: connect route with relief.
View question detailsTributaries in the Ganga system come from different source regions. Exam tip: check both source and confluence.
View question detailsA stream branching away in a delta is called a distributary. Exam tip: identify the term by flow direction.
View question detailsA river channel becomes shallower when sediment accumulates on its bed. This reduces the cross-sectional space available for water. During rainfall or a period of high discharge, the increased volume may not fit safely within the shallow channel. Water can then rise to the banks and spread across nearby low-lying land. Thus, a shallow bed can increase flood risk even when the additional water is not exceptionally large. Sediment deposition and reduced channel capacity are the important ideas.
Option A is correct because it connects a shallow bed with the spreading of water. The statement does not mean that every shallow river floods immediately; rather, shallow conditions make flooding more likely when discharge rises. Options B, C, and D are unrelated or impossible. A shallow bed does not dry the river, stop the sea, or turn the river into a volcano. In geographical reasoning, remember the sequence: more sediment in the bed → less channel capacity → higher water level and possible overflow.
Deposition in a delta can split the main river into many distributaries. Exam tip: remember delta and distributary together.
View question detailsChange in slope changes the direction of river erosion. Exam tip: understand vertical and lateral erosion.
View question detailsFresh deposits in flood plains can form fertile soil. Exam tip: write both benefits and harms.
View question detailsThe main tributaries of the Indus system include Jhelum, Chenab, Ravi, Beas and Sutlej. Yamuna, Ghaghara, Gandak and Kosi are important tributaries of the Ganga system. Option B incorrectly reverses these two groups. Narmada, Tapi, Godavari and Krishna belong to Peninsular river systems. Exam tip: memorise the sequence “Jhelum–Chenab–Ravi–Beas–Sutlej” for the Indus system.
View question detailsLong term deposition forms wide alluvial plains. Exam tip: connect northern plains with Himalayan rivers.
View question detailsBrahmaputra affects the physical and human geography of Assam. Exam tip: study it with processes.
View question detailsA perennial river helps in planning water use. Exam tip: connect water source with human use.
View question detailsThese places explain Ganga's course and processes in order. Exam tip: connect places with river route.
View question detailsYoung Himalayan slopes make river erosion strong. Exam tip: understand the link between young mountains and sediment.
View question detailsWhen velocity decreases the river deposits sediment. Exam tip: connect delta with slow flow and deposition.
View question detailsFlood planning requires understanding the whole catchment. Exam tip: connect basin with water management.
View question detailsQuestions on Himalayan rivers are often relation based. Exam tip: connect place and process together.
View question detailsHimalayan rivers are linked with many processes from source to delta. Exam tip: keep an overall view.
View question detailsHimalayan rivers erode in the upper course and deposit sediment in the lower course. Exam tip: understand the river with its full course and processes.
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