upied an 
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ng multi 
00 m at 
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ht bank 
>;d this 
ffecting 
. of the 
ibilgaon 
data of 
vidth of 
aon has 
ept few, 
on have 
of the 
changed 
iflux of 
each of 
may be 
ignment 
erefore 
)on i.e. 
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ve been 
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| vanish 
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AC-UP 
idance. 
al and 
nancial 
IAPRS & SIS, Vol.34, Part 7, “Resource and Environmental Monitoring”, Hyderabad, India, 2002 
support. Thanks are also due to Shri Alok Saini, Scientists, 
Shri P.K.Dey, Draftsman and Smt. Archana Singh, Typist for 
their kind cooperation. 
7. REFERENCES 
Bristow, C.S. (1993), Sedimentary structures exposed in bar 
tops in the Brahmaputra river, Bangladesh, Pub. in Braided 
rivers, Geo. Sol. Spl. Pub. 75, pp. 257-276. 
Chandsarkar, R.A. (1981), Change in river course in certain 
part of Brahmaputra, GSI Misc. Pub. 46 pp. 85-92. 
Doeglas, D.J. (1951), Meandering and braided rivers. Geol. 
Mijnbouw 9, 207-299. 
Fahnestock, R.K. (1963), Morphology & Hydrology of a glacial 
stretch: white river. Mount Rainier, Washington, USGS Prof. 
Pub. 422 A, A1A70. 
Lane, E.W., (1957), A study of the shape of channels formed by 
natural streams flowing in erodible material. MRD sediment 
series 9, U.S. Eng. Div., Omaha, NE. 
Oak, R.A. &. Appukuttan, V.K. (2001). Development and 
decay of channels in braided river - A study using remote 
sensing techniques. ICORG Proc. Spatial Technology 
Information, BS Pub. 2001, Vol..II, pp. 423-427. 
Roy Richardson, W. & Thorne, C.R. (2001), Multiple thread 
flow and channel bifurcation in braided river : Brahmaputra- 
Jamuna river, Bangladesh Jour. of Geomorphology, 38 (2001), 
pp. 185-196 
Schumm, S., (1960). The shape of alluvial chanels in relation 
to sediment type, USGS. Prof. Pap. 352-B, 17-30. 
Valdiya K.S. (1999). Why does river Brahmaputra remain 
untamed? Jour. of Current Sc., Vol-76, No.10, 25.5.1999. 
  
  
  
   
  
7 ^ 
STUDY AREA DZZAN 
Aromugge 
DHIMAYI 
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Figure - 1 Location Map of The Study Area