239 
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OO 
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\ 
43.7 
.0 
-402.7 
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” 
O’l” 
997 
982 
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1 
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3 
180.2 
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O’l” 
9 
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0’1” 
;s worse results 
the landslides, 
that relative to 
to interpolated 
■ous. Since one 
)f interpolation 
ribution of data 
culation of the 
nly those ones 
om the users), 
such parameter 
han the default 
>es not produce 
he residuals in 
0 m, while the 
tively. 
jad, in figure 2 
s to the DEMs 
1 the various 
it for SA20 are 
esults are also 
representation 
le data and the 
ipatible with 
th the dots is 
Figure 2 - SA20 landslide (scale 1:20.000). Post event input data.