Articles | Volume 13, issue 10
Nat. Hazards Earth Syst. Sci., 13, 2543–2550, 2013

Special issue: New developments and applications in early warning, monitoring...

Nat. Hazards Earth Syst. Sci., 13, 2543–2550, 2013

Research article 17 Oct 2013

Research article | 17 Oct 2013

Airborne geophysical survey of the catastrophic landslide at Stože, Log pod Mangrtom, as a test of an innovative approach for landslide mapping in steep alpine terrains

I. Baroň1,*, R. Supper2, E. Winkler2, K. Motschka2, A. Ahl2, M. Čarman3, and Š. Kumelj3 I. Baroň et al.
  • 1Karst and Cave Research Group, Department of Geology and Paleontology, Museum of Natural History, Museumsplatz 1/10, 1070 Vienna, Austria
  • 2Geological Survey of Austria, Neulinggasse 38, 1030 Vienna, Austria
  • 3Geological Survey of Slovenia, Dimičeva ulica 14, 1000 Ljubljana, Slovenia
  • *on leave: Geological Survey of Austria, Neulinggasse 38, 1030 Vienna, Austria

Abstract. Airborne geophysics is a promising method for investigating landslides. Here we present a case study of multisensor airborne geophysical survey at the catastrophic landslide Stože near Log pod Mangrtom in Slovenia, which was conducted in the framework of the European FP7th Project "SafeLand". Based on the survey itself and achieved results, we discuss applicability, limits, and benefits and costs of the method for investigating landslides in steep alpine terrains. Despite of several operational constraints, the airborne electromagnetic survey of the area well presented the lithological pattern and water saturation. The high resistivity regions mostly indicated drained slope scree and landslide mass, drained and loosened material of the moraine deposit in the tension zone of the landslide with present cracks and cavities. The minima of the resistivity pattern were attributed to the outcrop of marls rich in clay, to water-saturated moraine deposit above impermeable marls in the tension zone, and to water-saturated porous alluvial gravel and landslide scree along the Koritnica River. The magnetic survey proved to be inapplicable for such a small and rough area. The Potassium and Thorium maps, on the other hand, both well identified the regions of tension inside the landslide zone, outcrops of marls and dolomite, clay-rich colluvium, weathered zones along a regional tectonic fault, and alluvial deposits and deposits of debris flows, and the minima of the 137Cs clearly revealed the zones of material removal due to recent mass movements.