Geotechnical Distinction of Landslides Induced by Near-Field Earthquakes in Niigata, Japan

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geography/volume-2015/359047/figures/359047.fig.0012a.svgz" name="359047.fig.0012a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Nampei</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geography/volume-2015/359047/figures/359047.fig.0012b.svgz" name="359047.fig.0012b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Shiodani</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geography/volume-2015/359047/figures/359047.fig.0012c.svgz" name="359047.fig.0012c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Iketani</td></tr></table>

<div>Slope failures: upper row, before winter, and lower row, after snow-melting season.</div>

Geography Journal

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Figure 12

Figure 12: Geotechnical Distinction of Landslides Induced by Near-Field Earthquakes in Niigata, Japan 