Soil liquefaction due to Chi-Chi earthquake was found at Taichung harbor and several counties along the coast in Taichung. As a result of this strong earthquake occurred at the middle of Taiwan and the duration was long enough, the counties, Wufeng and Taiping, next to the western mountain areas also had serious damages due to soil liquefaction. Locations of soil liquefaction and corresponding damages in these two counties are investigated and described in this paper. There are several phenomena associated with soil liquefaction can be observed, they are sand blows, settlement and inclination of ground or buildings, lateral movement and spreading, and flow failure. The major places of sand blows are found to locate close to or beside the rivers, especially the sedimentation side of a river. The possible depths of liquefaction and soil properties are analyzed using collected boring log data and results of grain size distribution of the sand blow.