Darna River
Darna is a minor right-bank tributary of Godavari in the Nashik District, Maharashtra, India. Rising north of the Kalsubai range, it drains Igatpuri, Nashik and Niphad Talukas of Nashik District. The conjunction with Godavari is situated at Darnasangvi.
Origin
The Darna rises on the northern slopes of the Kulang hill fort in the Sahyadris about 13 km. south-east of Igatpuri.
Course
Though the straight line distance from the source to its confluence with the Darna is only about 50 km., it has a very long and winding course which measures about 80 km.[1] Its banks are like those of the Godavari below Nashik, of no great height, but broken by scores of small streams, making the passage along the banks of the river very difficult for laden carts. It is crossed by a bridge at Chehedi on the Nasik-Pune road, on the way to Sinnar. The bed is for the most part wide and sandy, though at times, the water flows over rocks. The Darna Dam is constructed across the Darna near Nandgaon village giving rise to the storage known as Lake Beale, which is visible for considerable distance while travelling by train from Mumbai to Nasik on the right hand side. This has enabled the construction of a pick-up weir on the Godavari river at Nandur-Madhmeshwar to divert the water into the Godavari canals.
On the right bank, at Belu, the river Darna receives the Kadva, not the large river of that name, but a small stream flowing north-eastwards between Mhordan-Katlia hills on the west and Kalsubai-Bitangad-Patta range on the east in the south-eastern part of Igatpuri taluka. On the left bank the Darna has only three tributaries of any size, and they hold little water during the hot season. They are the Waki, the Unduhol and the Valdevi.[2]
Tributaries
- Vaki: the Vaki nadi rises in the Dhoria hill and flows in a general southerly direction. The Tringalwadi Dam is located on the river. It passes between Igatpuri and Ghoti joins the Darna.
- Aaundha: the river is also spelt as Unduhol or Aund Vahal. It rises to the south of Anjaneri hill and flows in a south-easterly course. Here the river is impounded by the Mukane Dam. The reservoir waters turn in a northerly direction to the north of Kavnai hill, expelling the Aundha river to resume its easterly course before it joins the Darna just below the Darna dam.
- Waldevi: the Valdevi river comes to exist on the eastern slopes of the Anjaneri hill. It flows in a general easterly direction passing by Dadhegaon, runs through the outskirts of Nashik city and joins the Darna near Chehdi. It the longest tributary of Darna and joins it on the left-bank.
Dams
- Darna Dam
- Bhavali Dam
See also
External links
References
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Major tributaries | |
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Minor tributaries | |
Sub-tributaries |
- Jayakwadi Dam
- Majalgaon Dam
- Kaleshwaram Lift Irrigation Project
- Sriram Sagar Project
- Nizam Sagar
- Upper Wardha Dam
- Singur Reservoir
- Neher water system
- Dowleswaram Barrage
- Balimela Reservoir
- Devadula lift irrigation scheme
- Upper Dudhana Dam
- Godavari River Basin Irrigation Projects
- Pattiseema Lift Irrigation Project
- Sitamma Sagar Barrage
- Tummidihetti Barrage
- Sammakka Barrage
- Sadarmat Barrage
features / regions
Maharashtra | |
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Madhya Pradesh | |
Odisha | |
Chhattisgarh | |
Karnataka | |
Telangana | |
Andhra Pradesh |
- Khaparkheda Thermal Power Station
- Koradi Thermal Power Station
- Chandrapur Super Thermal Power Station
- Wardha Warora Power Plant
- Lanco Vidarbha Power Plant
- Nashik Thermal Power Station
- Dhariwal Power Station
- RattanIndia Nashik Thermal Power Station
- Kothagudem Thermal Power Station
- Kakatiya Thermal Power Station
- Parli Thermal Power Station
- NTPC Ramagundam
- NTPC Mauda
- Ramagundam B Thermal Power Station
- Tiroda Thermal Power Station
- Butibori Power Project
- Heavy Water Plant, Manuguru
- Waluj MIDC
- Shendra MIDC
- Shendra – Bidkin Industrial Park
- Ballarpur Industries
- HAL Sunabeda
- NALCO Damanjodi
Highways and railways |
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Bridges on Godavari |
river basin's sustainable
productivity & ecology
- Algal bloom in reservoirs
- High alkalinity of river water in the river basin upstream of Pochampadu dam
- Frequent floods in tail end area of the river basin
- Alkali salts / high pH water run off from ash / red mud dumps of coal fired power stations / bauxite ore enrichment
- Excessive silting of reservoirs due to deforestation and mining activities