[1] It was the source of the 1912 Shan state earthquake when it ruptured for a length of 160 km along the northernmost segment.

The Kyaukkyan Fault Zone's northernmost segment runs 160 km just north of Taunggyi and terminates east of Mandalay.

In 1912, the entire Myint Nge segment ruptured and produced an earthquake of magnitude 7.7.

The Kyaukkan Fault continue its trace for another 170 km, crossing the Myanmar-Thailand border, terminating north of Bangkok.

The 1988 Yunnan-Shan and 2011 Tarlay earthquakes were the most recent large events in the region.