Repeated renewal of Khadar soil is linked with which river condition?
Khadar forms from fresh deposits in flood plains. Exam tip: remember Khadar as new and fertile alluvium.
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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.
Khadar forms from fresh deposits in flood plains. Exam tip: remember Khadar as new and fertile alluvium.
View question detailsErosion may dominate upstream and deposition downstream. Exam tip: connect river courses with processes.
View question detailsIn plains the river forms winding courses. Exam tip: connect meanders with slow flow and lateral erosion.
View question detailsA large basin can receive more water and tributaries. Exam tip: connect basin size with floods.
View question detailsTributaries supply water and sediments to the main river. Exam tip: connect river network with large river systems.
View question detailsNorthern rivers may come from the Himalayas and southern rivers from Peninsular highlands. Exam tip: remember source regions.
View question detailsThe Hooghly, also called the Bhagirathi-Hooghly channel, is a distributary in the lower deltaic region of the Ganga. A distributary branches away from the main river and carries water towards the delta, whereas a tributary joins the main river. Therefore, Hooghly should not be identified as a tributary of the Ganga. Exam tip: a river branch that leaves the main channel in a delta is a distributary.
View question detailsHigh sediment can deposit in delta and form branches. Exam tip: connect sediment with delta development.
View question detailsGanga and Brahmaputra deposit towards the Bay of Bengal. Exam tip: connect the delta with the bay.
View question detailsAn alluvial fan forms where a river carrying sediment leaves a steep mountain valley and reaches a flatter area. The sudden reduction in slope causes the river to lose speed and transporting power. It then spreads outward and deposits gravel, sand, and finer material in a fan-shaped body, commonly near the foothills. The fan may have several shallow branching channels because the river changes course across its deposits. The amount and shape depend on sediment supply, water flow, and local relief.
The correct choice is A: when the river leaves the mountains and the slope suddenly decreases. This condition encourages deposition because the river can no longer carry all its sediment efficiently. The other choices do not provide the necessary change in slope and sediment movement. A river rising from the sea is not the normal setting, a sediment-free river cannot build an alluvial fan, and a river does not become a volcano. The key link is steep slope to gentle slope plus deposition.
In plains the river slows down and may deposit sediments. Exam tip: connect reduced velocity with deposition.
View question detailsAlluvial soil is fertile and supports farming in northern plains. Exam tip: connect river deposits with agriculture.
View question detailsThe Indus system is linked with both India and Pakistan. Exam tip: remember its tributaries and regional location.
View question detailsRiver character changes as relief changes along its course. Exam tip: connect route with relief.
View question detailsKhadar and Bhangar are both types of alluvial deposits found in the northern plains, but they differ mainly in age and position. Khadar is newer alluvium deposited by rivers during relatively recent floods. Fresh deposits can renew nutrients and often make Khadar fertile and agriculturally valuable. Bhangar is older alluvium found on higher terraces, so it is not renewed as frequently by annual floods and may have different soil properties.
Option A is correct because it connects Khadar with new deposits and possible renewal of fertility. Khadar does not form in the sea, Bhangar is not a glacier, and neither type is necessarily lava soil. The word “can” is important because actual agricultural value also depends on drainage, texture, salinity, and management. Still, the basic school-geography distinction is clear: Khadar is newer floodplain alluvium, while Bhangar is older alluvium.
A stream joining the main river is called a tributary. Exam tip: observe joining and branching directions.
View question detailsA stream branching away in a delta is a distributary. Exam tip: connect distributary with delta.
View question detailsHimalayan river plains provide water and fertile soil. Exam tip: connect river plains with agriculture and settlement.
View question detailsDuring monsoon more water enters rivers with rainfall. Exam tip: connect floods with season and water sources.
View question detailsHimalayan rivers get water from glaciers and rainfall while Peninsular rivers are more rain fed. Exam tip: remember water source difference.
View question detailsQUIZ COMPLETE