COMPARISON WITH FRACTUREYS KNOWN 
FROM THE GEOLOGICAL MAP 
The geological map of Yugoslavia (1:500,000) and the manu- 
Script geological map of Macedonia (1:200,000) were used in 
this correlation. Results were the following: 
- The faults seen in field, which control the general 
distribution and relations of units, can be detected on the 
Scanogram only if dividing areas of different albedo and 
texture. They control the relief and drainage in only a 
small percentage. 
- Two main space-observed systems are renegant to the 
older fabric and cannot be kinematically related with it. 
- Being closely related kmkk to the present relief and 
renegant to the older fabric, space-observed fracturos 
should be regarded as neotectonic features. 
These results may directly influence further imagery 
interpretation of the Balkan Peninsula. If accepted, they 
would point to the conclusions that the analysis of scano- 
grams: 
- may give relativi little data on fractures of geotectonic 
importance, if they do not represent boundaries of domains 
differing in albedo and texture, 
- may give sufficiently important minerogenic keys only 
if ore-controlling fractures are young enough to be 
mirrored in the relief, and 
- might be very important in neotectonic and seismotectonic 
studies. 
COMPARISON WITH THE 
PHOTOGEOLOGIC MAP 
Several years ago present authors with other members of the 
Laboratory for Methods of Geological Mapping (LMGK), Beograd, 
made a photogeological map of the whole of the SR of