Full text: Technical Commission IV (B4)

  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B4, 2012 
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia 
channel was produced by using ASTER DEM data in order to 
study the ancient river channel changes, terraces and banks (see 
Lónnqvist et al., 2007). In addition, the project has produced 
several satellite image analyses which reveal the 
geomorphology. Besides identifying the palaeolake depression 
of Nadra from Landsat-7 ETM image by cluster analysis and 
studies on the ground, the project has analysed the movement of 
the extending sand cover and explosive desertification in the 
area of Jebel Bishri (Lónnqvist et al., 2011). 
3. THE INTERRELATIONS BETWEEN 
THE WESTERN PLAINS AND THE MOUNTAIN 
3.1 The Oasis of El Kowm as a Base Camp 
The oasis of El Kowm (Fig. 4.) on the western piedmont of the 
mountain lies ca. 450 m above sea level and is situated in a 20 
km wide mountain pass. The basin is a little over 400 m lower 
from the peak of Jebel Bishri. It obviously served also as a base 
camp for the early hunter-gatherers, who were foraging and 
hunting in the region of Jebel Bishri. Long-term site formation 
processes took place in the oasis. In this arid landscape early on 
dozens of springs have attracted animals to the oasis, and 
human occupation in the area probably covers ca. 1 million 
years (Le Tensorer et al, 2007). Dozens of prehistoric sites 
(see Fig. 5.) have been traced in the region (see e.g., Besancon 
et al., 1981). 
At the western edge of Jebel Bishri a semicircular escarpment is 
called Tar al-Sbai (Fig. 4.) according to the Bedouin tribal 
border of the Sba'a tribe. Tar al-Sbai is facing the El Kowm 
oasis that is situated on the western plains beneath. The 3D 
image of the El Kowm and Tar al-Sbai area can be captured 
and flown over by GoogleEarth 3D at  35?11'05,66" N, 
38550'11,80"' E. The relationship of these two areas becomes 
more visible. 
  
Figure 4. The oasis of EI Kowm and Tar al Sbai at the edge of 
Jebel Bishri. Mapping on Landsat-7 ETM image by M. 
Lónnqvist 2001. 
The area of Tar al-Sbai comprises several abris, rock-shelters, 
of early hunter-gatherers that obviously frequented from the El 
Kowm basin up to the mountain proper. According to the finds, 
the visits to the area already started during the Palaeolithic era, 
but the greater utilization of the district is identified in the lithic 
workshops associated with abris dating from the Upper 
Palaeolithic and Epipalaeolithic eras. (Lónnqvist and Tôrmä, 
2003; Lónnqvist et al., 2011). The visits extended as far as the 
palaeolake of Nadra in the central area of the mountain during 
the Middle Palaeolithic period. During the Epipalaeolithic the 
emergence of the Natufian culture along the improvements in 
climatic conditions and population growth ca. 13, 000 BP. 
apparently developed in greater control of resources which led 
to territorialism (Bar-Yosef, 1998). 
  
Figure 5. Prehistoric sites in the El Kowm basin displayed on a 
Landsat-7 ETM image. Mapping on Landsat-7 ETM image by 
M. Lännqvist 2009, basing information on Besançon et al., 
1981. 
  
Figure 6. A computerized 3D landscape scene towards Tar al- 
Sbai from SW from the mosaic of Landsat-4 MSS images. Note 
the visibility to the Euphrates valley behind. Constructed by M. 
Tôrmä 2006. 
Because of their height and good visibility, the sites at Tar al- 
Sbai may simply be interpreted as lookout-points or 
observation-points at the mountain edges to control the 
surrounding steppe and desert plateau. From the edge, the 
approaching visitors could be seen and information could be 
spread. Lookout-points or observation-points are usually such 
that they provide extensions of the horizon for the field of 
vision in several directions. There are speculations concerning 
the things that are beyond the horizon, and in the human minds 
an extension of the horizon brings satisfaction (Appleton, 1975). 
In 2001 we already carried out computer-aided vision analyses 
from the mountain edge towards the western desert plateau 
using Russian topographic maps and Image Drape (Fig. 7. 
Lónnqvist et al., 2001 in press). Later on a vision analysis Was 
carried out over the western plain by fusing Landsat image data 
with ASTER DEM data (Fig. 8.). 
Our hypothesis is that visions and vistas were not only enjoyed 
because of their impressive values at the edge of the mountain 
but also due to practical considerations in connection with 
gazelle hunting and pastoral grazing. (Lónnqvist and Tórmà, 
2003; Lónnqvist et al., 2011). 
426 
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