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Fig. 8 | Swiss Journal of Geosciences

Fig. 8

From: The Chironico landslide (Valle Leventina, southern Swiss Alps): age and evolution

Fig. 8

Synthesis of subsurface data in the vicinity of the Chironico landslide, shown on a profile along the bottom of Valle Leventina, from northwest to southeast. Note that not all the cores are located exactly on the line of profile, thus several were projected into the profile plane. The red line represents the topography of the valley bottom; the thick brown line is a projection of the upper surface of the landslide into the profile plane. Vertical exaggeration is 15×. A–A′ and B–B′ are cross sections through the northern and southern depositional lobes of the landslide (for location, see Fig. 7). On the cross sections, the blue line is present valley topography whereas the red line is modelled landslide topography

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