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Peninsular Drainage System

The peninsular drainage system is older than the Himalayan drainage system as the peninsular river is a largely graded shallow valley....

The peninsular drainage system is older than the Himalayan drainage system as the peninsular river is a largely graded shallow valley.

Evolution of peninsular drainage system:

Three geological events shaped the drainage system:

  • Subsidence of western part of peninsular undersea in the tertiary period.
  • The upheaval of the Himalayas and the northern part of peninsular subsidence.
  • Tilting of the peninsular block from northwest to southeast direction leads to the flow of drainage system towards the Bay of Bengal.
  • River system;
East Flowing river or river discharging in the bay of Bengal:

The following are the east-flowing river from north to south:

  • Damodar river
  • Subarnrekha
  • Brahmani
  • Mahanadi river
  • Godavari river
  • Krishna river
  • Penner
  • Polar
  • Ponnaiyar
  • Cauvery river
  • Vaigai

Peninsular River System

  • Narmada:
    • It is the largest west flowing river of the peninsular region flowing through a rift valley between the Vindhya (north) and the Satpura Range (south).
    • It rises from Maikala range near Amarkantak in Madhya Pradesh.
    • Major Tributaries of the river are Hiran, Orsang, Barna and Kolar.
    • The Narmada basin covers parts of Madhya Pradesh, Maharashtra and Gujarat.
      • The Sardar Sarovar Project has been constructed on this river.
  • Tapi:
    • Another important westward flowing river, originates from the Betul district of Madhya Pradesh in the Satpura ranges.
    • It flows in a rift valley parallel to the Narmada but is much shorter in length.
    • Its basin covers parts of Madhya Pradesh, Gujarat and Maharashtra.
  • Mahanadi:
    • It rises in Raipur district of Chhattisgarh and runs through Odisha to discharge its water into the Bay of Bengal.
    • 53% of the drainage basin of this river lies in Madhya Pradesh and Chhattisgarh, while 47% lies in Odisha.
    • Major tributaries: Seonath, Hasdeo, Mand, Ib, Jonking and Tel rivers.
    • Its basin is bounded by the Central India hills on the north, by the Eastern Ghats on the south and east and by the Maikala range on the west.
  • Godavari:
    • It is the largest Peninsular river system and is also called the “Dakshin Ganga”.
    • It rises in the Nasik district of Maharashtra and discharges its water into the Bay of Bengal.
    • Its tributaries run through the states of Maharashtra, Madhya Pradesh, Chhattisgarh, Odisha and Andhra Pradesh.
    • Penganga, Indravati, Pranhita, and Manjra are its principal tributaries.
  • Krishna:
    • Krishna is the second largest east flowing Peninsular river which rises near Mahabaleshwar in Sahyadri.
    • Koyna, Tungbhadra and Bhima are its major tributaries.
    • It flows through the states Maharashtra, Karnataka, Telangana and Andhra Pradesh before flowing into the Bay of Bengal.
  • Kaveri:
    • Kaveri rises in Brahmagiri hills of Kodagu district in Karnataka.
    • It is a sacred river of southern India.
    • Its important tributaries are Arkavathi, Hemavathi, Bhavani, Kabini and Amravati.
    • It flows in a southeasterly direction through the states of Karnataka, Kerala and Tamil Nadu and drains into Bay of Bengal through Pondicherry.

Significance of Peninsular Drainage

  • The Peninsular rivers exclusively acquire water from rainfall, and water flows in these rivers only during the rainy season. As a result, these rivers are either seasonal or non-perennial.
  • As a result, these rivers are far less suitable for irrigation.
  • The Peninsular rivers exclusively acquire water from rainfall, and water flows in these rivers only during the rainy season.
  • The rivers of the Peninsular travel through rather shallow valleys. These are valleys that have been graded to some extent. There is little erosional activity in the rivers.
  • Estuaries are formed by several Peninsular rivers, such as the Narmada and the Tapi.
  • Deltas are formed by other rivers such as the Mahanadi, Godavari, Krishna, and Cauvery.
  • Several minor streams running westward from the Western Ghats join the Arabian Sea without forming a delta.
  • The plateau’s hard granite surface and non-alluvial composition leave limited room for the creation of meanders. As a result, the rivers of the Peninsular Plateau have very straight courses.

Read Also : Himalayan Drainage System

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