Full text: Remote sensing for resources development and environmental management (Volume 2)

636 
Figure 3. SPOT-HRV FCC of the northern Chott el 
Djerid, the road can be seen traversing the chott. 
The areas of aeolian activity (a), aioun (b) and 
salt crust (c) are easily identifiable. 
Figure 5. Landsat MSS FCC of the Sebkhet el Hamma 
from 1981. The detail in the chott has been 
increased by contrast stretching the chott at the 
expense of the surrounding areas but El Hamma (EA) 
can still be seen. Vegetation and salt patterns 
relating to surface water flow from the surrounding 
uplands is seen funnelling through the neck of the 
sebkhet as it enters the Chott El Fedjadj to the west. 
REFERENCES 
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1057-64 
Bird, A.C., Williams, T.H., Barrett, M.E., Munday, 
T.J. and Townshend, J.R.G. 1982 The Imperial 
College multi-channel electronic image classifier 
and its applications to the classification of 
Figure 4. Landsat TM (right) and SPOT-HRV (left) 
FCC's from 1983 and 1985 respectively showing 
sedimentation of alluvial fan material onto the 
northern chott el Djerid from a fan flanking theDjebel 
el Asker. There has been little change in the small 
sediment fan in the time between image acquisition. 
Figure 6. SPOT-HRV FCC image of part of the Chott el 
Djerid, March 1986. Two features are noticeable 
(i) the variable size of the aioun in the east of 
the image and (ii) the multiple flow-like features 
in the thin salt crusts, with cross-cutting 
relationships in the south-west, due to surface 
water flow. 
surface types by multispectral analysis Proc. 
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