International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part BS. Istanbul 2004 
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Figure 9. Residuals in elevation between kinematic GPS points | 
and photogrammetric edited DTM in the temenos area | The w 
(GPS minus photogrammetry, value in m). | in arc 
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3.2 Orthomosaicing | benefi 
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ATE products are suitable for the generation of orthophotos and | Digita 
orthophotomosaics, very interesting tools for documentation of DT 
and conservation of Cultural Heritage due to their capability to | tool f 
combine  metrical information with a qualitative and | tests i 
photographic description of the objects. potent 
For the studied site, as already underlined, a post-editing | specia 
process of the photogrammetric DTM was however necessary in | every 
areas with particular problems of homogeneous texturing or data a 
with sharp height variations. The orthophotos, characterized by | fundaı 
a ground pixel size of 20 cm, were obtained by using bilinear | the ir 
transformation as resampling method, and, in a unique step, | orthor 
mosaicked together obtaining the orthophotomosaic showed in | This 1 
figure 10, relative to the area surrounding the ‘emenos and the | to the 
dromos. in Cul 
The availability of large scale aerial imagery could be a mean to | 
integrate and complement terrestrial survey. The comparison 
(figure 11) between orthophoto and vector representation | 
coming from a topographical terrestrial survey conducted by the | 
archacologists, both into the same reference system, confirm a Aber, 
very good agreement and furthermore exemplifies the | forma 
possibility of recognizing by the image the structures not easily high r 
identifiable by a terrestrial survey (see in the middle-right of the | XXXI 
image). Conversely, it must be stressed that direct on-the-field Fieurc 10. Orthophotomoseic for the ara | | 
examination of semi-buried structures by the archaeologist surreundins thezenenos andithe dranos: Barati 
could provide in other cases a better interpretation. T | Digit 
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