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Tien Shan Geohazards Database: Landslide susceptibility analysis

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Fig. 3.Morphology of the Central Tien Shan and North-East Fergana Basin with outlines of landslides (dots, polygons) and scarps (thick dark lines); rivers, lakes and reservoirs are shown as well as active faults (see legend)
Fig. 4. Graphs of normalised landslide densities with respect to various factors: simplified geology (a: soft and hard rock) over Kyrgyzstan and Tajikistan, (pixel-based and number-based, considering also only slopes N5°); the altitude and average annual pr
Fig. 6. Combined fault (see black lines) — Mw ≥ 6.5 earthquake (circles, note for most large earthquakes an hypocentral depth of 10 km is adopted according to available seismological data) distance map (see text for explanation), colours indicating distanc
Fig. 8. Map of differences between the MGRP and the MGRP + E + F landslide susceptibility maps (here, only shown for Central Tien Shan and Fergana Basin)
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