Drainage System | Class 11 Geography Notes
By ConceptScroll Team · Published on 17 July 2026 · 3 min read

Drainage System – this guide gives you a concise, exam-ready overview of Drainage System from Class 11 Geography, written by ConceptScroll editors and reviewed against the latest NCERT textbook.
Drainage System
Drainage refers to the flow of water through well-defined natural channels such as rivers, nalas, and smaller streams that drain excess water during the rainy season. These channels play a crucial role in preventing large-scale flooding by efficiently carrying away surplus water. When these channels are ill-defined or blocked, flooding becomes a common and destructive phenomenon. The flow of water through these channels is called 'drainage', and the entire network of such channels in a region is known as a 'drainage system'. The drainage pattern of an area is influenced by several factors including the geological time period, the nature and structure of rocks, topography, slope, the amount of water flowing, and the periodicity of the flow.
A river drains water collected from a specific area called its 'catchment area'. The area drained by a river and its tributaries is known as a 'drainage basin'. The boundary line separating one drainage basin from another is called a 'watershed'. While river basins cover large areas, watersheds are relatively smaller catchment areas. Both river basins and watersheds are units of hydrological unity, meaning that what happens in one part of the basin affects the entire basin. This makes them important units for micro, meso, or macro-level planning.
Drainage patterns describe the arrangement of rivers and streams in a particular area and are influenced by the underlying geological structure and topography. The main drainage patterns include:
(i) Dendritic Pattern: This resembles the branches of a tree and is the most common drainage pattern. Rivers of the northern plains are examples.
(ii) Radial Pattern: Rivers originate from a central hill and flow in all directions. The rivers originating from the Amarkantak range are examples.
(iii) Trellis Pattern: Primary tributaries flow parallel to each other and secondary tributaries join them at right angles. This pattern is common in folded mountain regions.
(iv) Centripetal Pattern: Rivers discharge their waters from all directions into a central lake or depression.
Understanding drainage patterns helps in studying river behavior, flood management, and planning water resources.
📊 Diagram: 11954060; You have observed water flowing through the rivers, nalas and even channels during rainy season which drain the excess water. Had these channels not been there, large-scale flooding would have occurre; Figure 3.1 : A River in the Mountainous Region
🧪 Activity: Identify drainage patterns such as dendritic, radial, trellis, and centripetal in the topo sheet given in Chapter 5 of Practical Work in Geography-Part 1 (NCERT).
🔗 Connection: This section introduces the concept of drainage and drainage patterns, leading to the classification and overview of the Indian drainage system.
Frequently asked questions
Which of the following statements are correct? Assertion (A): The amount of moisture in the atmosphere is associated with latitude. Reason (R): The ability to keep the moisture in the form of water vapour is related to temperature
Both (A) and (R) are true, and (R) is the correct explanation of (A).
Which one of the following options is the most suitable way to solve the problem of floods and drought in India?
Transferring water of the perennial water basins to the water deficit river basins.
Which one of the following options justifies the naming of the river Kosi as ‘Sorrow of Bihar?
The Kosi deposits the carried sediments in the plains and changes its course frequently.
Match List -I with List-II and select the correct answer using the codes given below the list. Answers are in Alphabetical order List-I List-II A. Frost 1. Moisture deposited in the form of water droplets on cooler Surfaces like stones, grass blades. B. Dew 2. Frozen droplets and refrozen melted snow C. Sleet 3. Rain drops turning into ice pellets and coming down on the surface. D. Hailstones 4. Condensation takes place below freezing point on cold surfaces.
b. 4 1 2 3
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