region of the district is situated in Wardha-Vainganga valleys. All rivers are originated
from various mountains peaks and Satpuda hill ranges at Northern side. Except the part of
Wardha and Vena rivers all are temporary type
In Deoli, Wardha, Seloo, Hinganghat and
Samudrapur Tahasil the Drainage pattern is of Dendritic type. Where as in Karanja, Ashti,
Arvi Tahasil it is of Parallel or sub-parallel type. This is due to the controlling of
Joint-planes in Besalt on the flow routes of northern side rivers. Therefore various
northern side rivers flows parallel to the main river in North-South direction.
Wardha- Wardha river
originates on 785 meter high Multai plateau of Satpuda near Betul from where it travels
towards South and reaches in Wardha district. Further it flows at the North, West and
South boundaries of district and enters in Chandrapur district.
A Dam is constructed with mud age under the
Lower Wardha Project near Dhanodi village.
Vena- This is a main sub
Pothra- Pothra river
originates at south-east side of Girad hills at 390 Meter height. In 1982, a clay Dam is
constructed near Zunka village in Samudrapur Tahasil.
BorThis is also the
Dham Dham river is a
sub river originates on 465 meter high Brahmanwada hills of Dhaga, a reserved forest
region. It flows through various routes.
Panchdhara- This river is
Yashoda Yashoda is a
Bakli It originates
on 435 meter hight of Satarpur reserved forest region in Ashti Tahasil and joins river
Wardha at western side of Pargothan (Rly.) station.
Kar Kar river originates on 650 meter hight of north-east side of Kondhali. Later it joins river Wardha at its entry point in district.