The earthquake produced shaking at Pangandaran ( where the M6 .3 2006 Yogyakarta earthquake was felt more strongly ) of intensity III – IV ( '' Weak '' – '' Light '' ) , intensity III at Cianjur , and II ( '' Weak '' ) at Yogyakarta . Further inland and farther from the epicenter , intensity IV shaking made tall buildings sway in Jakarta , but at some coastal villages where many of the casualties occurred , the shaking was not felt as strong . An informal survey of 67 people that were present at the time revealed that in at least eight cases , individuals stated that they did not feel the earthquake at all ( a typical M7 .7 earthquake would have been distinctly noticed at those distances ) . The unusually low felt intensities , along with the short period body wave magnitudes , were components of the event that narrowed its classification into that of a tsunami earthquake
2006 Yogyakarta earthquake
2006 Yogyakarta earthquake
2006 Pangandaran earthquake and tsunami