mo gemza-
ain degree
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. ' TEXTURAL CLASSIFICATION : ^
TERRAIN MAPPING AFTER
STRUCTURE ANALYSIS
r:*E:ï!3K.
VÎÏ 4-
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Fig. 3a - Detail of central part of Fig. 2a.
Fig. 3b - Textural homogenization of Fig. 3a.
Homogenization is done by using the degree of resemblance
between the different textural classes.
- Fresh waters (l, Vaccares Lake; 2 , dark blue, deep
waters; 3 , light blue, shallow waters).
- Swampy areas (4, green, covered with vegetation;
5, brown, without vegetation)o
- Sea waters ( 6 , 7i 8 )o