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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

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Figure

Fig. 1. Stože landslide: (A) location of the test site, (B) generalsettings of the site with geology modified after Petrica and Špaca-pan (2001) and Jurkovšek (1987) and mapped faults (full blacklines) and with faults interpreted from topography (dot-and-da
Fig. 2. Photos of the test site: (A) the accumulation zone with di-amictic material of the landslide, (B) minor landslides above theplace, where the major landslide transformed into the debris flow,and (C) upper part of the landslide with bare surface of th
Fig. 4. Map of subsurface resistivity from the AEM survey, fault andjoint pattern (black full and dot-and-dashed lines), area of reliabledata (light grey dot-and-dashed line) and the geological interpre-tation (Source of data: Geological Survey of Austria and GoogleEarth).
Fig. 5. Map of magnetic anomalies combined with the fault andjoint pattern (black full and dot-and-dashed lines), and area of reli-able data (light grey dot-and-dashed line) (Source of data: Geologi-cal Survey of Austria and Google Earth).
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