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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