Articles | Volume 8, issue 4
Nat. Hazards Earth Syst. Sci., 8, 779–788, 2008
https://doi.org/10.5194/nhess-8-779-2008
Nat. Hazards Earth Syst. Sci., 8, 779–788, 2008
https://doi.org/10.5194/nhess-8-779-2008

  30 Jul 2008

30 Jul 2008

Ground deformation detection of the greater area of Thessaloniki (Northern Greece) using radar interferometry techniques

D. Raucoules1, I. Parcharidis2, D. Feurer1, F. Novalli3, A. Ferretti3, C. Carnec1, E. Lagios4, V. Sakkas4, S. Le Mouelic5, G. Cooksley6, and S. Hosford1 D. Raucoules et al.
  • 1BRGM, French Geological Survey, Orléans, France
  • 2Harokopio University of Athens, Department of Geography, Athens, Greece
  • 3Tele-Rilevamento-Europa, Milano, Italy
  • 4NKUA, Department of Geophysics & Geothermics, Athens, Greece
  • 5Université de Nantes, Nantes, France
  • 6NPA Group, Edenbridge, Kent, UK

Abstract. In the present study SAR interferometric techniques (stacking of conventional interferograms and Permanent Scatterers), using images from satellites ERS-1 and 2, have been applied to the region of Thessaloniki (northern Greece). The period covered by the images is 1992–2000. Both techniques gave good quantitative and qualitative results. The interferometric products were used to study ground surface deformation phenomena that could be related to the local tectonic context, the exploitation of underground water and sediments compaction.

The city of Thessaloniki shows relatively stable ground conditions. Subsidence in four locations, mainly in the area surrounding the city of Thessaloniki, has been detected and assessed. Two of the sites (Sindos-Kalochori and Langadhas) were already known from previous studies as subsiding areas, using ground base measurements. On the contrary the other two sites in the northern suburbs of Thessaloniki (Oreokastro) and in the south-east (airport area) were unknown as areas of subsidence. A further investigation based on fieldwork is needed in these two areas. Finally, an attempt to interpret the observed deformation, according to the geological regime of the area and its anthropogenic activities, has been carried out.

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