Full text: Proceedings, XXth congress (Part 7)

it still 
energy 
l'OE of 
erative 
energy. 
'cted to 
change 
h Tehri 
intry at 
try are 
ood the 
ints are 
ffected 
itation. 
ing the 
in. The 
| cover, 
system, 
ities of 
niseries 
around 
; “land” 
r It is 
nes and 
uilding 
but has 
; means 
— 
    
   
E 
a 
+ 
  
  
— Báüà RA 
| (after 
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
  
1.2 Force of Action 
The selection of suitable alternatives site for the rehabilitation 
of uprooted native people forms the basis of present study. 
2. ENVIRONMENTAL IMOPACTS ENVISAGED 
The study area whose geographical extents are shown in figure 
] lies around 30°45’N and 78°S0’E consisting of an area of 
about 2500 Km in the inner belt of Central Himalayan Region. 
Social and environmental impacts of this large dam have been a 
cause of concern over the last one decade as the dam is in the 
proximity of an active Srinagar Thrust (Prasad and Rawat, 
1986). The evidence suggested that the elites living far from the 
dam site will enjoy the benefits of the irrigation and power, it is 
the indigenous people who with low social status and little 
potential power will suffer the negative effects of dam. In 
addition to the anticipated increase in the incidence of water- 
borne disease such as the debilitating schistosomiasis 
(nilharzias), malaria and onchocerciasis (river blindness). Other 
potential costs which can be triggered by the construction of 
this dam in the geologically sensitive area are the economic 
costs of submergence of valuable resources such as fertile land, 
lumber and medicinal plants and the loss of hardwoods and 
biological resources. Therefore, while selecting the alternative 
site nearby for the displaced people, the scientific knowledge of 
the soil, its stability and the ecological balance of the selected 
site will permit the appropriate eco-friendly use of the land. 
3. INVESTIGATION PROCEDURE 
The published topographic cultural / physiographic map by the 
Survey of India at 1 : 50000 scale is used to prepare the base 
map and the land set TM data obtained from IRS LISS II of 
November 11, 1993 is being used as remote sensing output. 
The geological map of the area is digitized at original mapping 
scale of 1 : 50,000 and the areas if misties have been solved 
using remote sensing data. The maps have been generated in 
Polyconic projection system having Everest Ellipsoid for 
30°45°N Latitude and 78°50’E Longitude. 
Such special data maps in the form of topography, hydrology, 
geology, soil types, forest/land cover stored as layers in digital 
form in the computer. And finally, the presentation of results 
based on the outcome of comparing/overlaying the spatial data 
with different sets of features, their distribution in space and 
actual field checks. 
4. RESULTS AND DISCUSSIONS 
The Indian Space Program has been developed with multi facet 
vision for using space technology and the agriculture being the 
foremost. The Indian Remote Sensing Satellite (IRS) picture 
LISS-II offers the valuable dissemination of information on 
improved land, soil, water, vegetation utilization capabilities. 
The field checks show the variation of slopes from 100-300 
m/km having southern aspect. The soil is of alluvial type 
containing soil moisture of about «20 to 4076 on an average. 
The soil is of clayey to sandy loam type having moderate 
quantity of organic matter. 
On the basis of false color composite (FCC), figure 2 has been 
generated from the digitized data of Derhadun and is 
surroundings covering an area of about 2500 Km between the 
two major river the Yamuna in the west and the Ganga in the 
east, in order to demarcate various themes distinguishable from 
different colors. The red color covering and area of about 1500 
  
543 
Km? shows the forest envelope at higher altitudes (more than 
2300m above sea level marked with A and B) which is vital for 
man, plant and animals, fulfilling the basic needs of fuel 
fodder, manure, medicines and raw materials for industries. 
The plant area (marked with X,Y and Z), the yellow color 
depicts the agricultural area of about 700 Km? where the soil is 
very fertile having the moderate organic content. The green and 
orange color together shows the plantation of various kind 
covering an area of about 350 Km?. The Urban area is very less 
and the area covered by the water is about 20 Km” shown in 
blue color. 
Towords Tehri Dom 
7, 
River Gongo 
Fig. 2 Land Cover Themes — IRS LISS-II November 1993 
5. CONCLUSION 
Therefore, based on the latest available remote sensing 
information on water and land resources, integrated with the 
GIS provides an insight for planning the rehabilitation of about 
50,000 uprooted people from Upstream which is about 60 Km 
North-East of Dehradun city, can be thought of, without 
endangering the existing environment. 
6. ACKNOWLEDGEMENTS 
The author is grateful to various local agencies who have 
helped him during field checks. Several useful discussions were 
held with the Staff of Garhwal Vikas Mandal, Derhadun during 
the preparation of this paper. The help rendered by the staff is 
thankfully acknowledged. 
7. REFERENCES 
Pearce, F (1996) Superdams - have their attractions been 
overshadowed? Journal of Geosciences and development No. 
3, pp 7-10 
Prasad, C. and Rawat, G.S. (1986) Studies in recent 
reactivation along the Srinagar Thrust. Garhwal Himalaya 
Proc. Inter. Symp. Neotectonics in South Asia, Survey of India, 
Dehradun pp 301-312. 
Saxena, P.B., Bishnoi, Antium, Bhatia, D.K. and Saxena 
Bhuwan (1998) Investigations of eco-restorations of the 
Asarori - Mussoorie water divided to twin water sheds (Suswa- 
Asan) in the Derhadun Jr. Himal. Inst. of Action Research & 
Development, pp 19-29. 
Tiwari, R.S. and Garg, P.K. (1995) Land form and Land uses of 
Doon Valley and their role in resource development. Jr. 
Himalayan Geology, Vil. 6(2), pp 9-15. 
Valdiya, K.S. (1997) High Dams in Central Himalaya in 
context of active faults seismicity and societal problems. Jr. 
Geol. Soc. of India, vol. 49, pp 479-497. 
i 
H 
  
TT en 
 
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.