Hao-Cha village suffered from several typhoons and heavy rains since August 7, 2007. Those events caused the landslides in the northern part of Hao-Cha village and induced the occurrence of debris flows from the eastern part. That would damage the elementary school, partial houses and churches in that region. In view of the points, this study utilized 3S technology to qualitatively and quantitatively analyze certain debris hazard type. In the meantime, pilotless plane equipments were to take pictures around the damaged village and those pictures would help us to understand the suffering situation of landslide after the hazards attacked. From the results, the resistant shear strength would be reduced due to continuous heavy rain events and then the large scale landslide was to happen promptly in the northern part. The landslide deposited mainly in back basketball court of Hao-Cha elementary school. The height of deposition would decrease progressively from the northern part of slope to Ai-Liao south river. The typhoons and heavy rains brought much water and deposition in the river and make the river silted up so that The height of deposition almost equaled in that of the revetment. After all, the river courses generally belonged to the silted-up phenomenon and those phenomenon showed significantly especially in Ai-Liao south river.