Full text: Proceedings of the international symposium on remote sensing for observation and inventory of earth resources and the endangered environment (Volume 3)

    
  
   
   
  
  
  
   
UND TRUTH 
1AMETERS 
isurements 
“HED CARDS 
  
  
  
  
in the 
rally 
iere 
1976), 
.uding 
'oblems, 
jisary 
--wheel- 
. about 
20 man-months (counting the scientists only) were spent in the 
field for sampling, measuring sections, spectral reflectance 
measurements and checking out the geological interpretations. 
LANDSAT imagery was purchased from the US Geological Survey's 
EROS Center in Sioux Falls in the form of positive film 
transparencies at a scale of 1:1 ooo ooo and computer compa- 
tible digital tapes. The visual interpretation was done on 
1:500 ooo positive transparencies since earlier experiences 
had convinced us that this was the optimum scale (LIST, 
ROLAND & HELMCKE 1974; LIST & PÓHLMANN 1975; LIST, HELMCKE, 
MEISSNER, PÓHLMANN & ROLAND 1978). Mostly spectral bands 
7 and 4 were used; the latter especially for mapping the dune 
fields the knowledge of which proved very advantageous in the 
field for picking the best routes for travel. The interpreta- 
tion was plotted with special ink on transparent film so no 
details of the transparencies were lost. 
From the LANDSAT 1:500 ooo transparencies a controlled mosaic 
was assembled to fit the LAMBERT-GAUSS conical projection as 
used in the topographic maps "World 1:500 ooo Series 1404", 
from which some control points and information on names and 
altitudes were taken. This mosaic formed the topographic base 
on which the colored interpretation map was printed. 
In the original LANDSAT imagery it was sometimes difficult to 
discriminate between similar lithological units. So additional 
image processing techniques had to be used to extract more in- 
formation. 
Of all LANDSAT scenes color composites were produced by 
printing the spectral bands 4, 6 and 7 on yellow, cyan and 
magenta Diazo films and superimposing them to color subtractive 
composites. These proved very useful where small differences 
in spectral reflectance of rocks had to be distingushed; for 
instance, light colored limestone outcrops in many cases 
showed up in the same grey tone as sand in band 7. On the 
color composites, they could easily be separated by their 
   
  
  
  
  
  
   
  
  
  
  
  
   
   
  
  
  
  
  
  
   
   
    
   
    
	        
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