Dendrogeomorphology is now playing an important role in the study of geomorphic processes because of such characteristics tree ring have: accurately dating, high resolution and long time span. Some previous researches have shown that tree rings can be used as a reliable tool for historical evidence of past landslides, which can explain what is happening now and detect landslide deformation in the future. The paper reviewed the current situation and achievements of landslide studies which use dendrogeomorphological methods, especially the principles, the reconstruction of landslide activity and spatio-temporal distribution were illuminated. Finally, the shortcomings of this method were pointed out and the future development prospects were looked forward to.