anbul 2004 
'ology, land 
ion factors 
fferent level 
Erosion rate 
Less 
Medium 
High 
Very high 
process is in 
gy and steep 
'n and south- 
pe, less dept 
? presence of 
uth due to 
ates are very 
n, watershed 
mplemented. 
1 conjunction 
be useful to 
STAC model 
diment yield 
e processing 
ntly used for 
time point of 
st effective in 
studies. The 
jf using GIS 
using image 
ds in Erosion 
Erosion and 
ophys. Union, 
Sedimentation 
Engineering 
ork. 
Relationships 
| yield, Report 
International Archives of the Photogrammetry, Remote Se 
of the Task Committee on Sedimentation of the Hydraulics 
Division, J. Hydraul. Div.. Am. Soc. Civ. Eng., LOSCHY 11): 1328 
1365. ‘ 7132 
Su-Chin Chen, 2002. "The Assessment of soil erosion potential by 
SEIM in Taiwan", Warsaw, http:/kiki.baw.de/ conferences/ 
ICHE/ 2002-warsaw/ARTICLES/ PDF/242 pdf. S/ 
Heydarian,S.A.1996. " Assessment of erosion in Mountain 
regions", http://www.gisdevelopment.net/aars/acers/. 1996/. ts10/ 
ts10006pf.htm s10; 
Tajbakhsh, SM. and Memarian, 2003 H.. "the sediment yield 
potential estimation of Faridabad and Kordian watersheds using 
MESIAC is model in GIS framework", 
hitp://www.gisdevelopment.net/application/agriculture/soil/ma03 I 
S6pf.htm : 3 
1117 
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