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 Nepalese rivers
can be grouped into three categories on the basis of their
origin
(1) antecedent to Himalaya,
(2) after the Mahabharat. and
(3) after the Churia range.
Antecedent rivers belong to the period prior to the rise of the
Himalaya. These rivers added their tributaries during or after
the Himalayan origin alongwith the developement of monsoon
climate. After the formation of Mahabharat hills, the antecedent
rivers changed their courses as Mahabharat stood as a barrier.
As a result, most of the rivers changed their courses either to
the east or west. Most of these rivers were responsible to
deposit the sediments in the Churia basin.
The major river systems namely the Koshi, the Karnali and the
Gandaki belong to the antecedent group. Rivers originating from
the Mahabharat range and cutting through Churia hills come under
the second group, these include Kankai, Bagmati, Kamala etc. The
third group of rivers originate from the southern face of the
Churia hills. For the purpose of commercial rafting, the
following rivers are in use.
1. Saptakoshi River System (East Nepal)
2. Narayani or Saptagandaki River System (Central Nepal)
3. Karnali River System (West Nepal)
Eleven rivers in the three river systems are open for tourists
for rafting. The rivers are:
The Trishuli (Trisuli-Narayanghat)
The Kali Gandaki (Kusma-Tiger Tops)
The Bheri (Birendranagar- Chisapani)
The Seti (Damouli-Tiger Tops)
The Sunkoshi (Baseri-Chatara)
The Karnali (Karaleghat-Chisapani)
The Tama Koshi (Busti-Chatara)
The Arun (Tumlingtar-Chatara)
The Budhi Gandaki (Arughat-Trishuli)
The Bhote Koshi (Kodari-Lartza Bridge)
The Marshyangdi (Ngadi-Bimalnagar)
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