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This document summarizes the results of a geological engineering review and analysis of the mechanisms of rock mass movements caused by the 2006 earthquake in Yogyakarta, Indonesia. Over 150 rockslides and rockfalls were recorded in steep volcanic rock slopes in the western and northern parts of the Southern Mountains. One major NE-SW trending fault and associated microfaults controlled the stability of rock masses, leading to rock falls and slides. The largest event occurred at a slope of tuffaceous sandst

Author

Windu Nur Mohamad

Language

EN