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.
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Classification of surface sediments in Kuwait
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Bird, A.C., Williams, T.H., Barrett, M.E., Munday,
T.J. and Townshend, J.R.G. 1982 The Imperial
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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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