Full text: XVIIth ISPRS Congress (Part B4)

ng 
it 
  
GEOLOGICAL MAPPING IN ARID REGIONS OF AFRICA USING SATELLITE DATA - 
INTEGRATION OF VISUAL AND DIGITAL TECHNIQUES 
Franz K. List, Wolfgang Koch and Mohammad H. Salahchourian 
Freie Universitát Berlin, Institute of Geology, Geophysics and Geoinformatics 
D-1000 Berlin 46, Malteserstr. 74-100, Germany 
ABSTRACT 
Landsat-MSS data were used for preparing a geological map of entire Egypt at a scale of 1 : 500 000 in 20 sheets. This 
endeavor comprised production of optimized imagery for visual interpretation and field checks, as well as creation of digital 
mosaics of the whole country for base maps. Geometric control points were obtained during geologic field work from Transit 
satellites. Landsat-TM data, utilized in a present project in northeastern Sudan, provide improved spectral discrimination and 
higher spatial resolution. Color-ratio imagery is used for detection of gossans and gold-bearing quartz veins. Satellite, field, and 
elevation data are input into a GIS together with geophysical and petrologic data. Classification of lithology and subsequent map 
production is significantly improved by the integration of these information levels. 
1. INTRODUCTION 
Since the launch of ERTS-1 opened "a new window on our 
planet" (Williams & Carter, 1976) in July, 1972, geologists 
have made extensive use of the geometric and thematic 
information provided by the digital image data of Landsat 
MSS and TM. Landsat MSS data with their coarser resolution 
are a good choice for regional geologic analysis, both for 
structural as well as for lithologic investigations. TM data, on 
the other hand, provide improved information on spectral 
anomalies and smaller terrain features. From the beginnings 
of remote sensing, visual interpretation techniques familiar 
from "photogeology" were used for deriving information from 
the image data. With the growth in computer power and 
availability during the last decade, digital data processing sig- 
nificantly increased the quality of image representation, clas- 
sification and geometric accuracy. In this way, remotely 
sensed data can be operationally employed for regional geo- 
logic mapping and exploration, especially in arid and little ex- 
plored areas. 
2. MAPPING IN EGYPT 
After preliminary studies on applications of early Landsat-1 
imagery to small-scale geologic interpretation in the Tibesti 
Mountains, Chad, resulting in a satellite interpretation map 
(List, Roland & Helmcke, 1974; List, Helmcke, Meifàner et 
al., 1978), a pilot project was started in Egypt using stan- 
dard image interpretation methods for preparing a first geo- 
logic map of southwestern Egypt at 1 : 500 000 scale (List 
et al., 1982, 1984). In this project, the image data used for 
interpretation were MSS standard products in the form of 
photographic data. 
Any interpreter who has worked with these early standard 
products has made the experience that the image quality was 
not really good enough for proper identification of geologic 
details or minor spectral differences in lithology. Also the 
image geometry was not up to map standards even at small 
scales. 
Thus in 1981 a mapping project was started in cooperation 
with CONOCO with the intention to produce a geologic map 
of entire Egypt at 1 : 500 000 that would conform to inter- 
national mapping standards. The map was to consist of 20 
sheets covering an area of 2° by 3° each. The following ob- 
jectives were set for the final map: 
325 
® To produce geometrically corrected digital mosaics as a 
map base guaranteeing topographic accuracy; 
® To adopt a format of the map sheets conforming to the in- 
ternational World Map grid; 
® To carry out adequate field work to be able to properly 
classify and correlate the sedimentary and basement 
rocks; 
® To perform the geologic interpretation and compilation on 
high-quality color composite imagery for best results; and 
€ To complete the entire project possibly within 6 years. 
2.1 Geologic setting and map philosophy 
Egypt is an arid country with an area of more than 1 million 
km? (see fig. 1). Only 396 of the land surface, namely the 
Nile valley and the Delta, are covered by vegetation. 
  
SES Mediterranean :*. 
  
  
  
  
Fig. 1: Sketch map showing Egypt and the actual 
study area in Sudan. 
 
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.