Full text: Proceedings, XXth congress (Part 3)

  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B3. Istanbul 2004 
  
2. ENVIRONMENTAL 
DEVELOPMENT OF THE REGION 
In the absence of deforestation, grazing or cultivation the 
modern climatic conditions would allow the vegetation typical 
of the Terebinth-Almond Woodland steppe in the region of 
Jebel Bishri. Changes in vegetation of the region took place 11 
000 to 10 000 years ago, when the drastic retreat of the 
woodland took place ca. 11 500 B.P. (See Moore et al., 2000). 
The continuous zone of forest has not reached the area for past 
ten thousand years, although occasional trees or small plots of 
woods have existed. Only earlier in the Palaeolithic Stone Age 
the area has obviously been greener exemplified by several 
wadis and terraces which offer plenty of archaeological remains 
of past human activities. 
Nowadays the mountain of Jebel Bishri itself is practically 
devoid of agriculture and constant combating against increasing 
desertification is under way by ACSAD (The Arab Centre for 
the Studies of Arid Zones and Dry Lands). During the past 
hundred years the ecological balance of this Syrian steppe has 
suffered major setbacks caused by grazing, gathering of 
firewood, agriculture and increasing traffic. However, the 
neighbourhood belongs to the perimeters of the so-called Fertile 
Crescent and the cradle of agriculture. Ca. 100 kilometers 
northwest from Jebel Bishri up the stream of the Euphrates lies 
Abu Hureyra, the oldest agricultural site in the world. It offers 
the earliest hither-to-known signs of domestication of cereals 
(rye) dated to ca. 9000 B.C., i.e., to the Epipalaeolithic Period 
by radiocarbon datings. Abu Hureyra is an important example 
of the change from the mobile hunter-gatherer way of life to 
sedentarization and the development of the village life. (See 
Moore et al. 2000). The oases of El Kowm and Qdeir on the 
western piedmont area of Jebel Bishri have offered comparable 
evidence of the sedentarization and nomadization processes of 
early humans. (See, e.g., Cauvin, 1982 and Zarins, 1989). 
In order to visually approach the environmental contrasts of the 
region the Finnish project SYGIS has used satellite data in 
constructing a 3-- model of the border zone representing the 
mountain and the alluvial zone of the Euphrates (see Figure 1.). 
Figure 1. The 3-D-model of Jebel Bishri and the Euphrates 
valley from the east. Construction by Markus Törmä, raw data 
copyright: DLR and Eurimage 
  
Monitoring changes from past to present in this environmental 
border zone opens vistas for human responses to the 
environment in space and time. Human groups have found 
different strategies. to adapt to marginal environments. These 
responses can be expressed in different economic and social 
898 
ways, and it is our task to delincate the responses in the 
archaeological record. 
But to avoid environmental determinism we ought to 
understand that people also alter the environment: e.g., 
agriculture — causes sedimentation — and over-grazing 
desertification. Different sources of satellite data from various 
years offer excellent possibilities to detect changes in 
desertification and river channel migration. Monitoring and 
comparing environmental changes through satellite data in 
different years elucidates the post-depositional processes and 
preservation of archaeological remains in the area. 
Understanding the change also offers us means to follow the 
development in the area, find new sites buried by environmental 
changes and to offer choices for planning new strategies of 
preserving traditional economies and culture in the area. 
3. DATA ACQUISITION, 
PREPROCESSING AND 
INTERPRETATION METHODS 
Remote sensing data utilized so far consists of optical satellite 
images and digital elevation models. 
3.1 Satellite images 
In order to determine the land cover of study area and its 
changes as well as visualization purposes, following remote 
sensing images have been acquired: 
e 4 Landsat Multi-Spectral Scanner (MSS) images, 
185/35 and 185/36 taken 27.6.1975 (Landsat 2) and 
172/35 and 172/36 12.7.1983 (Landsat 4) 
Downloaded from Global Land Cover Facility 
(http://glcf.umiacs.umd.edu/). 
e 2 Landsat Thematic Mapper (TM) images, 172/35 and 
172/36 taken 1.9.1990 (Landsat 4). Downloaded from 
Global Land Cover Facility (see the website above). 
e Landsat Enhanced Thematic Mapper image, path 172, 
row halfway 35 and 36, taken 29.1.1999. Acquired 
from Novosat Ltd. Copyright Eurimage. 
e  QuickBird pan-sharpened multispectral image, 
coordinate of the centre: lat. 35. 422, long. 39. 4788 , 
taken 15.7.2003. Acquired from Novosat Ltd. 
Copyright Eurimage. 
e. 3 CORONA images, taken 28.6.1966, 22.1.1967 and 
22.1.1967, places S FWD 1034-2, S FWD 1038-2 and 
S FWD 1038-2. Acquired from USGS. 
The spatial and spectral properties of these images are presented 
in Table 1. in the end of the article. 
Landsat is a series of polar orbiting remote sensing satellites. 
The first Landsat was launched 1972 and the last one, the 
seventh, 1998. The most important instruments onboard 
Landsat-satellites have been Multi-Spectral Scanner (MSS), 
Thematic Mapper (TM) and Enhanced Thematic Mapper 
(ETM). These instruments are electro-optical scanners which 
produce digital data (Kramer, 1996). The main differences are 
number of channels and their wavelengths and spatial resolution 
(see Table I in the end of the article). 
QuickBird is a modern digital imager with very high spatial 
resolution, less than 1 meter on panchromatic channel. There 
are also four multispectral channels (see Table 1 in the end of 
the article). Due to the high spatial resolution, the image size is 
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