NAVDANYA
 
Research Foundation for Science, Technology and Ecology (RFSTE)
 
Home Page
About Us
From the Founder, Mission, Vision, The Practice of Earth Democracy, organisation, Overview
News
Upcoming Events
Earth democracy
Seed sovereignty
Food sovereignty
Water sovereignty
Land sovereignty
Education for Earth Citizenship; Bija Vidyapeeth
Registration, Course fees, The Campus, Accommodation
Biodiversity and Organic Movement
Navdanya's Organic Movement
Navdanya's Organic Production
Navdanya's Organic products
Empowerment of Women and Children
Articles
Articles and Researches by Dr. Vandana Shiva and other authors.
Publications
Books written by Dr. Vandana Shiva and other authors.
Newsletter
Archives
Search
Contact Us
 

A preliminary Survey in the Bhagirathi Valley: Status of River Bhagirathi from Gangotri to Deoprayag

Introduction
The rocks of lesser Himalayan zone of the area are dominated by the metasedimentaries while the higher Himalayan zone is characterized by high grade crystalline rocks with frequent basic and acidic intrusions. The granitic rocks (Gangotri granites) are present the upper most reaches of the Bhagirathi catchment.  The North Almora Thrust (NAT), exposed near Nalupani in Bhagirathi valley, divided the Tehri Phyllites (Chnadpur Formation) from the quartzites of Garhwal Group. Near sainj, the Main Central Thrust (MCT) is present which separates the rocks of Garhwal Group (quartzites, slates, carbonates etc.) from the rocks of Central Crystallines (gneisses and schists).  
Gangotri Temple
Preliminary survey has been carried out through the course of the river Bhagirathi right from Devprayag to Gangotri. Main objective of this survey was to workout the current status of river Bhagirathi keeping in view that a number of Hydropower projects completed or under construction throughout the Bhagirathi River. In all three major hydroelectric power projects has been completed and two are under construction phase. In addition 3 mega projects are proposed one at Harshil, and 2 on Jad Ganga in Bhairav Ghati area (Table 1). On completion of on going and under construction project, there will be no more Bhagirathi river running right from Lohari to Koteshwar (near Tehri) covering an stretch of more than 125 Km. Besides to this, it would be a potential area of man made disaster in future. There are several evidences of adverse impacts (seen/observed) shortly within 1.5 years of completion of the Tehri dam.  

Major Bhagirathi Valley Hydro Power Projects at a glance: 

1.         

2.         

3.         

4.         

5.         

6.         

7.         

8.         

9.         

10.      

11.      

12.      

13.      

14.      

15.      

16.      

17.      

18.      

19.      

20.      

21.      

22.      

23.      

 

2a. Maneri Bhali Phase I have already been in operation from 1988. It is a run off river scheme, in which a small barrage was built at Maneri and water is diverted through a tunnel to powerhouse located 15 km downstream at Tiloth, Uttarkashi Town. Capacity of this powerhouse is 90 MW (45x45). Since past 10 years this Powerhouse has never generated electricity power to its full capacity. One of the reasons for low power generation has been repeated damage of turbine blade by the high-speed quartz mineral particles flowing with water.

 

2b. Manari-Bhali Phase II consists of a diversion barrage at Joshiyada-Gynsu Uttarkashi with its water level at 1404 m msl and a 304 MW capacity Powerhouse located 24 km downstream at Dharasu. This project has come in operation from January 2008. At present, this powerhouse is generating 102MW electricity only. A 16 km long tunnel has been constructed from Uttarkashi to Dharasu through left side of the river Bhagirathi. Whole river water is diverted to this tunnel for power generation at Dharasu. Water level is still low. 85 houses will drown if the reservoir in Uttarkashi if it stores water to its full capacity i.e. 1410m msl.