Question

Chandra and Bhaga the two streams join to form ______ river.
A. Jhelum
B. Indus
C. Ravi
D. Chenab

Answer 1

Hint: The drainage framework is a coordinated arrangement of feeders and a trunk stream that gather and channel surface water to the ocean, lake, or some other waterway. The course of action of streams in a locale, controlled by slope, varying stone protection from enduring and disintegration, atmosphere, hydrologic changeability, and underlying controls of the scene is known as a waste example. In this way, seepage design alludes to a plan in which a stream and its feeders structure together, from its source to its mouth.

Complete answer:
The Chenab River Basin is a major part of the Indus River Basin. This river is formed by the Chandra and Bhaga, rising in Lahul. It moves through Himachal Pradesh and Kashmir and is known as Chandra-Bhaga or Chenab. It at that point Traverses 330 km to Akhnur where it enters Pakistan. It streams 644 km more to Panjnad, joins the Sutlej after getting the eaters from Jhelum at Trimmu and the Ravi drop down, its catchment zone up to the Indo-Pakistan line is 26,155 sq km. Chandra and Bhaga the two streams merge to frame the Chenab river. Two streams specifically Chandra and Bhaga ascend on the contrary sides of the Baralacha pass at a height of 4,891 meters and meet at Tandi at a rise of 2,286 meters to frame the waterway Chenab. The Chenab ascends from the South-East and Bhaga from the North-West of the Baralacha pass.

Thus, option (D) is correct.

Note: Himachal Pradesh has numerous perpetual snow-took care of waterways and streams, notwithstanding four significant conduits. The eastern segment of the state is depleted essentially by the Sutlej River, which ascends in Tibet. Depleting the western piece of Himachal Pradesh are the Chenab (Chandra-Bhaga), Ravi, and Beas streams, which have their source in the Great Himalayas.