Full text: Papers accepted on the basis of peer-reviewed abstracts (Part B)

406 
In: Wagner W., Szdkely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010,1 APRS, Vol. XXXVIII, Part 7B 
Figure 16. Church of St. Peter of Alcantara and its vicinity 
in an orthophoto from 2003 
Aerial photos also help to identify the process of abandonment 
in originally agricultural areas which being disused gradually 
turn into semi-natural areas. 
3.2 Forestation 
In most cases, the process of abandonment is succeeded by the 
process of forestation in which abandoned areas overgrow with 
self-seeded vegetation in the first phase followed by a 
subsequent gradual transition to forest stands. 
3.3 Submersion 
Submersion represents a process of the change of artificial 
surfaces, agricultural areas, forests and semi-natural areas into 
water bodies. New water surfaces originate primarily as related 
very closely to mining (tailings ponds) or secondarily as a 
consequence of undermining (submerged ground subsidences). 
Aerial photo time series facilitate the identification of the 
process from both spatial and temporal points of view (Figure 
17). 
Figure 17. The area before (year 1947, © MO CR/GeoSI ACR) 
and after (year 2003) the occurrence of a submerged 
ground subsidence 
4. CONCLUSION 
The aerial photo analysis of the effects of mining on landscape 
showed that both direct and indirect signs must be taken into 
consideration in visual photointerpretation. In order to identify 
the primary and secondary displays of mining activities stress is 
put on direct signs contained in a respective photo: shape, size 
tone, colour, texture and structure of an object. However, these 
signs must be complemented with the interpretation of indirect 
signs, i.e. logical signs that require deep knowledge on the 
research phenomena (Ciolkosz, Miszalski, Oledzki, 1999). 
Indirect signs used in the interpretation of anthropogenic 
landforms include particularly the location of an object and its 
relations to other objects in a photo. 
Unlike the primary and secondary mining displays, the 
processes are absent in the photos, however, they can be derived 
from multitemporal analysis of aerial photos. Such processes 
are presumed on the basis of indirect signs in combination with 
supporting information used in order to differentiate between 
mining-related processes and other processes that take place in 
the landscape. 
Correct interpretation of the displays of deep mining depends 
on interpreter’s direct experience with events taking place in the 
mining landscape. Subsequently, accurate visual interpretation 
of the displays of deep mining enables us to quantify the extent 
of changes, determine their direction and analyse processes in 
heavily anthropogenically-affected landscape. Aerial photos 
represent an important source of information in the study of 
territorial differentiation of changes, their intensity, character 
and causes. Complex understanding of these processes makes it 
possible to predict the landscape development and ecological 
and social consequences in the landscape affected by hard coal 
deep mining. 
5. REFERENCES 
Ciolkosz, A., Miszalski, J., Oledzki, J. R., 1999. Interpretation 
of aerial photographs. PWN, Warszawa, 458 p. (in Polish) 
Havrlant, M., 1980. Anthropogenic landforms and the 
environment in Ostrava industrial region. Pedagogical Faculty, 
Ostrava, 153 p. (in Czech) 
Jensen, J. R., 2006. Remote Sensing of the Environment. An 
Earth Resource Perspective. Pearson Education, Upper Saddle 
River, 608 p. 
Mulkova, M., Popelka, P., Popelkova, R., 2010. The Impact of 
Industrialization on the Landscape of the Ostrava-Karvina 
Mining District. Landscape Ecology - methods, applications 
and interdicsiplinary approach, (in press) 
OKD, a.s. (Ostrava-Karvina Mining District) [online] Available 
at: http://www.okd.cz/ 
PVS (Map service of the Portal of the Public Administration of 
the Czech Republic) [online] Available at: 
http ://geoportal .cenia.cz/ 
Zapletal, L., 1969. Introduction to anthropogenic 
geomorphology I. Palacky University, Olomouc. 280 p. (in 
Czech)
	        
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