What is one reason for large bends in the course of Himalayan rivers?
In plains gentle slope slows the river and forms bends. Exam tip: connect meanders with plain flow.
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SubjectsGeography
भारत की अपवाह प्रणालियाँ
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
Up to 20 questions from this page. Select your focus, then start.
In plains gentle slope slows the river and forms bends. Exam tip: connect meanders with plain flow.
View question detailsHimalayan rivers get water from rain and snow while Peninsular rivers depend more on rainfall. Exam tip: remember this main difference.
View question detailsThe general slope of the Deccan is eastward so many rivers enter the Bay of Bengal. Exam tip: link slope with flow direction.
View question detailsThe short distance between Western Ghats and the sea makes rivers flow on steep slopes. Exam tip: remember the narrow western coast.
View question detailsSutlej is a major tributary of the Indus system. Exam tip: remember Sutlej as a Punjab river.
View question detailsGhaghara and Kosi are major tributaries of the Ganga. Exam tip: connect rivers of the northern plain with the Ganga system.
View question detailsKosi is known for shifting course and floods. Exam tip: connect river course change with flooding.
View question detailsThe Brahmaputra is called Tsangpo in Tibet. Exam tip: remember different regional names of one river.
View question detailsRivers help provide irrigation water and alluvial soil. Exam tip: connect river plains with agriculture.
View question detailsRivers bring sediments and deposit them in plains. Exam tip: connect alluvial plains with deposition.
View question detailsCatchment area is the area that supplies water to a river. Exam tip: connect it with the idea of basin.
View question detailsMore tributaries increase the extent of a river system. Exam tip: connect tributaries with water collection.
View question detailsThe northern plains are formed by deposits of the Ganga Indus and Brahmaputra systems. Exam tip: connect northern plains with Himalayan river systems.
View question detailsPlateau slopes and hard rocks help form waterfalls. Exam tip: connect Peninsular plateau with waterfalls.
View question detailsFlow direction helps understand the final outlet of a river. Exam tip: separate east-flowing and west-flowing rivers.
View question detailsHimalayan and Peninsular river systems have different nature in India. Exam tip: study source slope and deposition together.
View question detailsAn antecedent river keeps cutting its course even after land uplift. Exam tip: connect it with deep valleys of Himalayan rivers.
View question detailsIn a parallel pattern streams flow almost in the same direction. Exam tip: connect it with steep slope.
View question detailsSabarmati and Mahi flow westward towards the Arabian Sea. Exam tip: remember them with Narmada and Tapi in the west-flowing group.
View question detailsThe Sundarbans are a major part of the Ganga-Brahmaputra delta. Exam tip: connect Sundarbans with delta and mangroves.
View question detailsQUIZ COMPLETE