The 1955 Yuzha earthquake (1955年鱼鲊地震) occurred on September 23, 1955, at 15:06 UTC (23:06 local time). The epicenter was located in the area around Lazha (拉鲊), Dalongtan (大龙潭) Township,

Renhe District Renhe District () is a district of the city of Panzhihua, Sichuan Province, China. It borders Huili to the east, Yongren County of Yunnan Yunnan; is an inland Provinces of China, province in Southwestern China. The province spans approxi ...

Panzhihua Panzhihua ( zh, c=攀枝花, p=Pānzhīhuā), formerly Dukou ( zh, labels=no, c=渡口), is a prefecture-level city located in the far south of Sichuan province, China, at the confluence of the Jinsha and Yalong Rivers. It has an administrative ...

and Yuzha (鱼鲊) Township, Huili County. Lazha then belonged to

Yongren County Yongren County (; Chuxiong Yi script: , ) is a county under the administration of the Chuxiong Yi Autonomous Prefecture, in the north of Yunnan province, China. It borders Huili, Sichuan across the Jinsha River to the east, Yuanmou County to the ...

Yunnan Yunnan; is an inland Provinces of China, province in Southwestern China. The province spans approximately and has a population of 47.2 million (as of 2020). The capital of the province is Kunming. The province borders the Chinese provinces ...

and now within

Sichuan Sichuan is a province in Southwestern China, occupying the Sichuan Basin and Tibetan Plateau—between the Jinsha River to the west, the Daba Mountains to the north, and the Yunnan–Guizhou Plateau to the south. Its capital city is Cheng ...

. Yuzha then belonged to Huili County, Sichuan as it still does. The earthquake had a magnitude of 6.8. 728 people were reported dead and 1547 injured in the earthquake. More than 15000 rooms collapsed. Eight people died and seven houses collapsed in the Xigeda (昔格达) Village. Cracks ranging from 10 to 70 cm in width and 100 to 1,500 m in length occurred on hillsides and ridges. Landslides were observed along both banks of the

Jinsha River The Jinsha River (, Classical Tibetan, Tibetan: Dri Chu, འབྲི་ཆུ, ) or Lu river, is the Chinese name for the upper stretches of the Yangtze River. It flows through the provinces of the PRC, provinces of Qinghai, Sichuan, and Yu ...

. Many villages on both banks of the Jinsha River were destroyed. Rivers and springs dried up, and many new springs appeared. Changes of water level in wells and ditches were reported. Many villages on both banks of the Jinsha River were destroyed. Along the Jinsha River and its surrounding gullies, large quantities of rocks broke, fell, and dammed up the gullies. In the Jinsha River, waves surged 1 m high. The maximum intensity reached MM IX. The shaking could be felt as far as about 400 km away. The Xigeda-Yuanmou fault (昔格达—元谋断裂带), about 270 km long, is the seismogenic structure of this earthquake."昔格达断裂晚第四纪活动特征及强震复发周期" by 卢海峰 and 姬志杰 From the distribution of the isoseismals of this earthquake, it was suggested that there is a three-layered structure. There is a rupture layer, and there are two complete rock layers located in both sides of the rupture layer. The rupture layer is the place where the stress was concentrated and released and has the role of reflecting the seismic wave propagation."中国强震发生带地震构造的几点思考" by 李坪, 黄广思, and 杨美娥

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* Yuzha earthquake, 1955 Earthquakes in Sichuan Earthquakes in Yunnan History of Panzhihua 20th century in Sichuan {{China-stub

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