Baitarani River

The Baitarani River recently surged past its danger mark, causing floods that impacted several low-lying villages in Bhadrak district of Odisha. This event has once again highlighted the challenges posed by river management, particularly in flood-prone areas.

About the Baitarani River:

Geography and Course:

• Origin: The river originates from the Gonasika Hills in Keonjhar district, Odisha, at an elevation of about 900 meters above sea level.

• The river's unique source is the Guptaganga stream, which flows underground before emerging, making it a sacred site for many.

• It flows primarily in an eastern direction after initially flowing northward. The river runs through both Odisha and Jharkhand and serves as the boundary between the two states at its upper course.

• Length: Approximately 360 km, the river ultimately drains into the Bay of Bengal.

Drainage Basin and Area:

• The Baitarani River Basin spans a total area of around 12,790 square kilometers.

• It is bordered by the following:

  • South and West: The Brahmani River basin.

  • North: The Subarnarekha River basin.

  • East: The Burhabalang River and the Bay of Bengal.

Major Tributaries:

• Baitarani has a network of 65 tributaries, with 35 coming from the left and 30 from the right side.

• Some key tributaries include:

  • Salandi, Gahira, Kusei, Deo, Kanjhari, Musal, Arredi, Siri, Kukurkata, Budhi, Ambajhara, and Remal.

Economic Significance:

• The basin is rich in both mineral and agricultural resources, making it an ideal area for industrial growth. The fertile delta formed by the river, alongside other rivers like the Mahanadi and Brahmani, is crucial for the local economy, supporting both agriculture and industry.

Flooding:

• The Baitarani River has been a source of flooding during the monsoon season, especially when the water level surges past its danger mark.

• The recent floods in Bhadrak district are a stark reminder of the vulnerability of many low-lying villages along the river, which often face inundation during periods of heavy rainfall and river surges.