17 March 2005 Kuzulu Landslide (Sivas/Turkey)(<Featured Articles>Turkey-Japan Joint Conference on Geomorphology)

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概要

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• The back-analysis results of the land slide (Kuzul Landslide) on 17 March 2005 (initial sliding in the source area) indicated that the most likely cause should be pore water pressure increase due to snow melting and thawing of the groundwater. It is also noted that on the basis of the interpretations on pre-event air photos/satellite images and information obtained from eye-witnesses, it is evident that the slope movements in the study area are continuously occurring for many years indicating their retrogressive character and the possibility of a future large landslide.

• 2011-04-25

著者

• Yigitbasioglu Hakan

  Faculty Of Language And History-geography Ankara University

関連論文

• 17 March 2005 Kuzulu Landslide (Sivas/Turkey)(Turkey-Japan Joint Conference on Geomorphology)
• Preface(Turkey-Japan Joint Conference on Geomorphology)

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